点苍山-哀牢山变质杂岩带中、北段多期花岗质岩浆事件及其构造意义
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摘要
点苍山-哀牢山变质杂岩带位于青藏高原东南缘扬子板块与印支板块的结合部位。杂岩带经历了多期构造-岩浆-变质事件的叠加,带内物质组成极其复杂,是研究古特提斯演化、印度-欧亚板块俯冲-碰撞-隆升以及渐新世印支地体沿红河-哀牢山左行走滑侧向挤出的关键地区。本文对点苍山-哀牢山变质杂岩带中、北段戛洒地区11件花岗质岩石进行了LA-ICPMS锆石年代学和岩石地球化学分析,研究揭示出新元古代、中三叠世、始新世和渐新世四期不同类型的花岗质岩浆活动。其中4件花岗质岩石中锆石206Pb/238U加权平均年龄为780.0±6.3Ma~743.6±6.7Ma,部分岩石内发育有渐新世深熔锆石;1件花岗质片麻岩内27颗锆石的206Pb/238U加权平均年龄为234.3±2.0Ma;3件花岗斑岩锆石U-Pb测年获得36.67±0.54Ma~33.01±0.39Ma的加权平均年龄;3件花岗质片麻岩/糜棱岩中获得渐新世(28.58±0.57Ma~24.53±0.29Ma)侵位年龄。岩石地球化学研究揭示新元古代花岗质岩石具有较高的Cu、V、Zn、TiO_2含量及较高铝指数,A/CNK变化范围为1.09~1.13,TiO_2含量为0.44~0.60;中三叠世花岗岩具有钙碱性特征,A/CNK<1.0,R1-R2图解中落入深熔花岗岩范围内;始新世花岗岩具有高Sr、Ba、K_2O含量,高Sr/Y、Sr/Nd、Ba/Th比值,低Nd、Na)2O含量的特点,岩石中全碱含量为9.2%~10.4%,Sr/Y值为48.8~94.5,Sr/Nd值为30.4~65.3,Ba/Th值为151~358;渐新世花岗岩全碱含量较低变化范围为3.25~9.03,A/CNK范围为1.09~1.14,属富铝质S型花岗岩。花岗质岩石野外产状、锆石年代学与岩石地球化学综合研究揭示新元古代花岗质岩石可能属扬子板块西缘原特提斯洋俯冲形成的陆缘岩浆弧,印支期造山作用过程中卷入到杂岩带内,新生代区域性走滑剪切使岩石进一步发生变形和深熔;中三叠世花岗岩为古特提斯洋闭合后扬子板块与印支板块碰撞后伸展构造热事件的响应;始新世花岗质岩石为印度-亚欧板块碰撞后伸展背景下地幔上涌交代下地壳进而产生的富钾花岗质岩石,且侵位年代由北向南逐渐变新记录了印度-亚欧板块汇聚角度的调整过程;渐新世花岗质岩石为红河-哀牢山剪切-走滑抬升过程中变沉积岩、新元古代和晚二叠世-三叠纪花岗质岩石的部分熔融而成。
The Diancang Shan (DCS)-Ailao Shan (ALS) metamorphic complex belt is located on the southeastern margin of Tibetan Plateau,which separated the Yangtze Block to the east and the Indochina Block to the west.The DCS-ALS complex belt consists mainly of various metamorphic rocks,and was overprinted on multiple deformation and metamorphism events,where is a key region for revealing the complicated evolution of the Paleo-Tethys,subduction-collision-exhumation between the Indian-Eurasian plate and the Indochina Block extrusion alone the Red River (RR)-Ailao Shan sinistral strike-slip shearing zone in Tertiary.In this study,eleven granitoid rocks are collected from the Gasa area within the north-middle segment of DCS-ALS metamorphic complex.Neoproterozoic,Mid-Triassic,Eocene and Oligocene four periods of granitic magmatism have been constrained by LA-ICP-MS dating.Thereinto,four granitic rocks yield the weighted mean206Pb/238 U ages ranging from 780.0 ± 6.3Ma to 743.6 ± 6.7Ma,indicating a Neoproterozoic magmatic event occurring in the southwestern margin of Yangtze Block.In contrast,27 zircons collected form one granitic gneiss yield the weighted mean206Pb/238 U ages of 234.3 ± 2.0Ma.Whereas three granitic rocks show the weighted mean206Pb/238 U age ranging from 36.67 ± 0.54 Ma to 33.01 ± 0.39 Ma.Three granitic mylonite yield the youngest Oligocene ages of 28.58± 0.57 Ma ~ 24.53 ± 0.29 Ma.Geochemical analysis of various granites have revealed that the Neoproterozoic granitic rocks are rich in Cu,V,Zn and TiO_2 content with a higher Al index.The value of A/CNK and the TiO_2 content change from 1.09 to 1.13 and 0.44 to0.60,respectively.The Mid-Triassic granitic gneiss with A/CNK rations < 1.0 belong to calc-alkaline series in SiO_2-K_2O diagram,and plot into the region of anatectic granitoids in R1-R2 diagram.The Eocene granitic/granodioritic rocks contain the total alkali contents ranging from 9.18 to 10.43 show higher Ba,Sr,K_2O contents,and lower Na2 O content with higher Sr/Y (48.8 ~ 94.5),Sr/Nd (30.4 ~ 65.3) and Ba/Th (151 ~ 358) ratios.The Oligocene granitic rocks have lower total alkali contents (3.25 ~ 9.03) and higher A/CNK ratios 1.09 ~ 1.14,which belong to typical S-type granite.Combine studies of the field occurrence,geochronology and geochemical features with previous published data have revealed the petrogenesis and tectonic evolution for the various granitic rocks within the Diancang Shan-Ailao Shan complex belt.The Neoproterozoic granitic rocks are similar to the continental arc granites which were genetically related to the Proto-Tethys ocean subduction to the southwestern margin of Yangtze Block,and subsequently involved in the DCS-ALS metamorphic complex during late collision orogeny.The Mid-Triassic granitic gneiss shows closly relationship with the post-collisional extension between Yangtze Block and Indochina Block.Post-collisional extension between Indian plate and Eurasia plate in Eocene triggered the potassic porphyry intruded in/around DCS-ALS area.The emplacement ages decrease from north to south reflect the the adjustment of convergence angel.The Oligocene granitic rocks are genetic connect to the RR-ALS regional strike-slip.The preexisted rocks in deep level within the complex zone were uplifted to shallow crust during strike movement and induce partial melting eventually formed the syn-tectonic granitic rocks.
The Diancang Shan (DCS)-Ailao Shan (ALS) metamorphic complex belt is located on the southeastern margin of Tibetan Plateau,which separated the Yangtze Block to the east and the Indochina Block to the west.The DCS-ALS complex belt consists mainly of various metamorphic rocks,and was overprinted on multiple deformation and metamorphism events,where is a key region for revealing the complicated evolution of the Paleo-Tethys,subduction-collision-exhumation between the Indian-Eurasian plate and the Indochina Block extrusion alone the Red River (RR)-Ailao Shan sinistral strike-slip shearing zone in Tertiary.In this study,eleven granitoid rocks are collected from the Gasa area within the north-middle segment of DCS-ALS metamorphic complex.Neoproterozoic,Mid-Triassic,Eocene and Oligocene four periods of granitic magmatism have been constrained by LA-ICP-MS dating.Thereinto,four granitic rocks yield the weighted mean206Pb/238 U ages ranging from 780.0 ± 6.3Ma to 743.6 ± 6.7Ma,indicating a Neoproterozoic magmatic event occurring in the southwestern margin of Yangtze Block.In contrast,27 zircons collected form one granitic gneiss yield the weighted mean206Pb/238 U ages of 234.3 ± 2.0Ma.Whereas three granitic rocks show the weighted mean206Pb/238 U age ranging from 36.67 ± 0.54 Ma to 33.01 ± 0.39 Ma.Three granitic mylonite yield the youngest Oligocene ages of 28.58± 0.57 Ma ~ 24.53 ± 0.29 Ma.Geochemical analysis of various granites have revealed that the Neoproterozoic granitic rocks are rich in Cu,V,Zn and TiO_2 content with a higher Al index.The value of A/CNK and the TiO_2 content change from 1.09 to 1.13 and 0.44 to0.60,respectively.The Mid-Triassic granitic gneiss with A/CNK rations < 1.0 belong to calc-alkaline series in SiO_2-K_2O diagram,and plot into the region of anatectic granitoids in R1-R2 diagram.The Eocene granitic/granodioritic rocks contain the total alkali contents ranging from 9.18 to 10.43 show higher Ba,Sr,K_2O contents,and lower Na2 O content with higher Sr/Y (48.8 ~ 94.5),Sr/Nd (30.4 ~ 65.3) and Ba/Th (151 ~ 358) ratios.The Oligocene granitic rocks have lower total alkali contents (3.25 ~ 9.03) and higher A/CNK ratios 1.09 ~ 1.14,which belong to typical S-type granite.Combine studies of the field occurrence,geochronology and geochemical features with previous published data have revealed the petrogenesis and tectonic evolution for the various granitic rocks within the Diancang Shan-Ailao Shan complex belt.The Neoproterozoic granitic rocks are similar to the continental arc granites which were genetically related to the Proto-Tethys ocean subduction to the southwestern margin of Yangtze Block,and subsequently involved in the DCS-ALS metamorphic complex during late collision orogeny.The Mid-Triassic granitic gneiss shows closly relationship with the post-collisional extension between Yangtze Block and Indochina Block.Post-collisional extension between Indian plate and Eurasia plate in Eocene triggered the potassic porphyry intruded in/around DCS-ALS area.The emplacement ages decrease from north to south reflect the the adjustment of convergence angel.The Oligocene granitic rocks are genetic connect to the RR-ALS regional strike-slip.The preexisted rocks in deep level within the complex zone were uplifted to shallow crust during strike movement and induce partial melting eventually formed the syn-tectonic granitic rocks.
引文
Batchelor RA and Bowden P.1985.Petrogenetic interpretation of granitoid rock series using multicationic parameters.Chemical Geology,48(1-4):43-55
Bureau of Geology and Mineral Resources of Yunnan Province.1990.Regional Geology of Yunnan Province.Beijing:Geological Publishing House,45-201(in Chinese)
Cai YF,Wang YJ,Cawood PA,Zhang YZ and Zhang AM.2015.Neoproterozoic crustal growth of the southern Yangtze Block:Geochemical and zircon U-Pb geochronological and Lu-Hf isotopic evidence of Neoproterozoic diorite from the Ailaoshan zone.Precambrian Research,266:137-149
Cao SY,Liu JL,Leiss B,Vollbrecht A,Zou YX and Zhao CQ.2009.Timing of initiation of left-lateral slip along the Ailao Shan-Red River shear zone:Microstructural,texture and thermochronological evidence from high temperature mylonites in Diancang Shan,SWChina.Acta Geologica Sinica,83(10):1388-1400(in Chinese with English abstract)
Cao SY,Liu JL,Leiss B,Vollbrecht A,Genser J,Neubauer F and Zhao CQ.2012.Initiation of left-lateral deformation along the Ailao ShanRed River shear zone:New microstructural,textural,and geochronological constraints from the Diancang Shan metamorphic massif,SW Yunnan,China.International Geology Review,54(3):348-367
Chen B,Long XP,Wilde SA,Yuan C,Wang Q,Xia XP and Zhang ZF.2017.Delamination of lithospheric mantle evidenced by Cenozoic potassic rocks in Yunnan,SW China:A contribution to uplift of the Eastern Tibetan Plateau.Lithos,284-285:709-729
Chen XL,Huang WT,Zou YQ,Liang HY,Zhang J and Zhang YQ.2016.Zircon U-Pb geochronology and geochemistry of ore-bearing porphyries in the southern Yulong porphyry copper belt,and factors resulting in the differences in scale of mineralization between the southern and northern Yulong porphyry copper belt.Acta Petrologica Sinica,32(8):2522-2534(in Chinese with English abstract)
Chung SL,Chu MF,Zhang YQ,Xie YW,Lo CH,Lee TY,Lan CY,Li XH,Zhang Q and Wang YZ,2005.Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism.Earth-Science Reviews,68(3-4):173-196
De la Roche H,Leterrier J,Grandclaude P and Marchal M.1980.Aclassification of volcanic and plutonic rocks using R1R2-diagram and major-element analyses:Its relationships with current nomenclature.Chemical Geology,29(1-4):183-210
Deng J,Wang QF,Li GJ and Santosh M.2014a.Cenozoic tectonomagmatic and metallogenic processes in the Sanjiang region,southwestern China.Earth-Science Reviews,138:268-299
Deng J,Wang QF,Li GJ,Li CS and Wang CM.2014b.Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region,SW China.Gondwana Research,26(2):419-437
Deng J,Wang QF,Li GJ and Zhao Y.2015.Structural control and genesis of the Oligocene Zhenyuan orogenic gold deposit,SW China.Ore Geology Reviews,65:42-54
Deng WM,Huang X and Zhong DL.1998.Petrological characteristics and genesis of Cenozoic alkali-rich porphyry in West Yunnan,China.Chinese Journal of Geology,33(4):412-425(in Chinese with English abstract)
Gao LE and Zeng LS.2014.Fluxed melting of metapelite and the formation of Miocene high-Ca O two-mica granites in the Malashan gneiss dome,southern Tibet.Geochimica et Cosmochimica Acta,130:136-155
Guan T,Huang ZL,Xu C,Zhang ZL,Yan ZF and Chen M.2006.Dating and geochemical characteristics of lamprophyres in the Baimazhai nickel deposit,Yunnan Province.Acta Petrologica Sinica,22(4):873-883(in Chinese with English abstract)
Guo LG,Liu YP,Xu W,Zhang XC,Qin KZ,Li TS and Shi YR.2006.Constraints to the mineralization age of the Yulong porphyry copper deposit from SHRIMP U-Pb zircon data in Tibet.Acta Petrologica Sinica,22(4):1009-1016(in Chinese with English abstract)
Guo ZF,Hertogen J,Liu JQ,Pasteels P,Boven A,Punzalan L,He HY,Luo XJ and Zhang WH.2005.Potassic magmatism in western Sichuan and Yunnan provinces,SE Tibet,China:Petrological and Geochemical constraints on petrogenesis.Journal of Petrology,46(1):33-78
He WY,Mo XX,Yu XH,He ZH,Dong GC,Liu XB,Su GS and Huang XF.2013.Zircon U-Pb and molybdenite Re-Os dating for the Beiya gold-polymetallic deposit in the western Yunnan Province and its geological significance.Acta Petrologica Sinica,29(4):1301-1310(in Chinese with English abstract)
Hu XJ.2012.Petrogenesis and geological significance of Cenozoic K-rich intermediate-acid plutons along Ailao Shan-Red River fault zone.Master Degree Thesis.Xi’an:Northwest University,1-73(in Chinese with English summary)
Jian P,Liu DY,Kr9ner A,Zhang Q,Wang YZ,Sun XM and Zhang W.2009.Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China(Ⅱ):Insights from zircon ages of ophiolites,arc/back-arc assemblages and within-plate igneous rocks and generation of the Emeishan CFB province.Lithos,113(3-4):767-784
Jin XD and Zhu HP.2000.Determination of 43 trace elements in rock samples by double focusing high resolution inductively coupled plasma-mass spectrometry.Chinese Journal of Analytical Chemistry,28(5):563-567(in Chinese with English abstract)
Lai CK,Meffre S,Crawford AJ,Zaw K,Xue CD and Halpin JA.2014a.The western Ailaoshan volcanic belts and their SE Asia connection:A new tectonic model for the eastern Indochina Block.Gondwana Research,26(1):52-74
Lai CK,Meffre S,Crawford AJ,Zaw K,Halpin JA,Xue CD and Salam A.2014b.The Central Ailaoshan ophiolite and modern analogs.Gondwana Research,26(1):75-88
Leloup PH,Arnaud N,Lacassin R,Kienast JR,Harrison TM,Trong TTP,Replumaz A and Tapponnier P.2001.New constraints on the structure,thermochronology,and timing of the Ailao Shan-Red River shear zone,SE Asia.Journal of Geophysical Research,106(B4):6683-6732
Li BL,Ji JQ,Fu XY,Gong JF,Song B,Qing JC and Zhang C.2008.Zircon SHRIMP dating and its geological implications of the metamorphic rocks in Ailao Shan-Diancang Mountain ranges,west Yunnan.Acta Petrologica Sinica,24(10):2322-2330(in Chinese with English abstract)
Li BL,Ji JQ,Fu XY,Gong JF,Song B,Qing JC,Zhang C and Ma ZJ.2009.Metamorphic times limits’study on the metamorphic rocks series of Ailao Shan-Diancang Mountain Ranges,West Yunnan.Acta Petrologica Sinica,25(3):595-608(in Chinese with English abstract)
Li BL,Ji JQ,Wang DD and Ma ZJ.2012.Neoproterozoic magmatism in South Yunan:Evidence from SHRIMP zircon U-Pb geochrological results of high-grade metamorphic rocks in the Yaoshan Group.Acta Geologica Sinica,86(10):1584-1591(in Chinese with English abstract)
Li GJ,Wang QF,Yu L,Hu ZC,Ma N and Huang YH.2013.Closure time of the Ailaoshan Paleo-Tethys Ocean:Constraints from the zircon U-Pb dating and geochemistry of the Late Permian granitoids.Acta Petrologica Sinica,29(11):3883-3890(in Chinese with English abstract)
Lin TH,Chung SL,Chiu HY,Wu FY,Yeh MW,Searle MP and Iizuka Y.2012.Zircon U-Pb and Hf isotope constraints from the Ailao Shan-Red River shear zone on the tectonic and crustal evolution of southwestern China.Chemical Geology,291:23-37
Liu C,Deng JF,Liu JL and Shi YL.2011.Characteristics of volcanic rocks from Late Permian to Early Triassic in Ailaoshan tectonomagmatic belt and implications for tectonic settings.Acta Petrologica Sinica,27(12):3590-3602(in Chinese with English abstract)
Liu FL,Wang F,Liu PH and Liu CH.2013.Multiple metamorphic events revealed by zircons from the Diancang Shan-Ailao Shan metamorphic complex,southeastern Tibetan Plateau.Gondwana Research,24(1):429-450
Liu FL,Wang F,Liu PH,Yang H and Meng E.2015b.Multiple partial melting events in the Ailao Shan-Red River and Gaoligong Shan complex belts,SE Tibetan Plateau:Zircon U-Pb dating of granitic leucosomes within migmatites.Journal of Asian Earth Sciences,110:151-169
Liu HC,Wang YJ,Cai YF,Ma LY,Xing XW and Fan WM.2013.Zircon U-Pb geochronology and Hf isotopic composition of the Xin’anzhai granite along the Ailaoshan tectonic zone in West Yunnan Province.Geotectonica et Metallogenia,37(1):87-98(in Chinese with English abstract)
Liu HC,Wang YJ,Fan WM,Zi JW,Cai YF and Yang GL.2014.Petrogenesis and tectonic implications of Late-Triassic highεNd(t)-εHf(t)granites in the Ailaoshan tectonic zone(SW China).Science China(Earth Sciences),57(9):2181-2194
Liu HC,Wang YJ,Cawood PA,Fan WM,Cai YF and Xing XW.2015c.Record of Tethyan ocean closure and Indosinian collision along the Ailaoshan suture zone(SW China).Gondwana Research,27(3):1292-1306
Liu JL,Song ZJ,Cao SY,Zhai YF,Wang AJ,Gao L,Xiu QY and Cao DH.2006.The dynamic setting and processes of tectonic and magmatic evolution of the oblique collision zone between Indian and Eurasian plates:Exemplified by the tectonic evolution of the Three River region,eastern Tibet.Acta Petrologica Sinica,22(4):775-786(in Chinese with English abstract)
Liu JL,Wang AJ,Cao SY,Zou YX,Tang Y and Chen Y.2008.Geochronology and tectonic implication of migmatites from Diancangshan,western Ynnnan,China.Acta Petrologica Sinica,24(3):413-420(in Chinese with English abstract)
Liu JL,Chen XY,Wu WB,Tang Y,Tran MD,Nguyen QL,Zhang ZCand Zhao ZD.2015a.New tectono-geochronological constraints on timing of shearing along the Ailao Shan-Red River shear zone:Implications for genesis of Ailao Shan gold mineralization.Journal of Asian Earth Sciences,103:70-86
Liu YS,Hu ZH,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Lu YJ,Kerrich R,Cawood PA,Mc Cuaig TC,Hart CJR,Li ZX,Hou ZQ and Bagas L.2012.Zircon SHRIMP U-Pb geochronology of potassic felsic intrusions in western Yunnan,SW China:Constraints on the relationship of magmatism to the Jinsha suture.Gondwana Research,22(2):737-747
Qi XX,Wang XH,Zhu LH,Hu ZC and Li ZQ.2010.Validation on age of Neoproterozoic intrusions from northeastern margin of Indochina block,western Yunnan and its tectonic implication:Evidence from zircon LA-ICP-MS U-Pb dating and geochemistry.Acta Petrologica Sinica,26(7):2141-2154(in Chinese with English abstract)
Qi XX,Santosh M,Zhu LH,Zhao YH,Hu ZC,Zhang C and Ji FB.2014.Mid-Neoproterozoic arc magmatism in the northeastern margin of the Indochina block,SW China:Geochronological and petrogenetic constraints and implications for Gondwana assembly.Precambrian Research,245:207-224
Qi XX,Santosh M,Zhao YH,Hu ZC,Zhang C,Ji FB and Wei C.2016.Mid-Neoproterozoic ridge subduction and magmatic evolution in the northeastern margin of the Indochina block:Evidence from geochronology and geochemistry of calc-alkaline plutons.Lithos,248-251:138-152
Searle MP.2006.Role of the Red River shear zone,Yunnan and Vietnam,in the continental extrusion of SE Asia.Journal of the Geological Society,163(6):1025-1036
Searle MP,Yeh MW,Lin TH and Chung SL.2010.Structural constraints on the timing of left-lateral shear along the Red River shear zone in the Ailao Shan and Diancang Shan Ranges,Yunnan,SW China.Geosphere,6(4):316-338
Shen SY,Wei QR,Cheng HL,Mo XX and Feng QL.2000.Two kinds of silicalites in Mount Ailao belt,Yunnan Province.Chinese Science Bulletin,45(23):2176-2180
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Tian G,Zhang CQ,Peng HJ,Zhou YM,Li JR,Zhang XP and Hu MY.2014.Petrogenesis and geodynamic setting of the Chang’an gold deposit in southern Ailaoshan metallogenic belt.Acta Petrologica Sinica,30(1):125-138(in Chinese with English abstract)
Wang DB,Tang Y,Liao SY,Yin FG,Sun ZM,Wang LQ and Wang BD.2013.Zircon U-Pb dating and its geological implications of the metamorphic rock series in Ailao Shan Ranges,western Yunnan.Acta Petrologica Sinica,29(4):1261-1278(in Chinese with English abstract)
Wang F,Liu FL and Liu PH.2011.Metamorphic evolution and anatexis of gneissic rocks in the Diancangshan-Ailaoshan metamorphic complex belt,southeastern Tibet Plateau.Acta Petrologica Sinica,27(11):3280-3294(in Chinese with English abstract)
Wang F,Liu FL and Liu PH.2013.Metamorphic evolution of metasedimentary rocks within the Diancang Shan-Ailao Shan metamorphic complex belt.Acta Petrologica Sinica,29(2):630-640(in Chinese with English abstract)
Wang F,Liu FL,Liu PH,Shi JR and Cai J.2016a.Petrology,geochemistry,and metamorphic evolution of meta-sedimentary rocks in the Diancang Shan-Ailao Shan metamorphic complex,Southeastern Tibetan Plateau.Journal of Asian Earth Sciences,124:68-93
Wang YJ,Zhou YZ,Cai YF,Liu HC,Zhang YZ and Fan WM.2016b.Geochronological and geochemical constraints on the petrogenesis of the Ailaoshan granitic and migmatite rocks and its implications on Neoproterozoic subduction along the SW Yangtze Block.Precambrian Research,283:106-124
Wang YZ,Li XL,Duan LL,Huang ZX and Cui CL.2000.Geotectonics and Metallogeny in the South Nujiang-Lancang-Jinsha Rivers Area.Beijing:Geological Publishing House,1-123(in Chinese)
Yumul GP Jr,Zhou MF,Wang CY,Zhao TP and Dimalanta CB.2008.Geology and geochemistry of the Shuanggou ophiolite(Ailao Shan ophiolitic belt),Yunnan Province,SW China:Evidence for a slowspreading oceanic basin origin.Journal of Asian Earth Sciences,32(5-6):385-395
Zeng LS,Gao LE and Xie KJ.2011.Concurrence of Mid-Miocene high Sr/Y granite and leucogranite in the Yardoi gneiss dome,Tethyan Himalaya,Southern Tibet.Mineralogical Magazine,75(3):2245
Zhang JJ,Zhong DL,Sang HQ and Zhou Y.2006.Structural and geochronological evidence for multiple episodes of deformation since Paleocene along the Ailao Shan-Red River shear zone,southeastern Asia.Chinese Journal of Geology,41(2):291-310(in Chinese with English abstract)
Zhang Q,Zhou DJ,Zhao DS,Huang ZX,Han S,Jia XQ and Dong JQ.1994.Ophiolites of the Hengduan Mountains,China:Characteristics and tectonic settings.Journal of Southeast Asian Earth Sciences,9(4):335-344
Zhang Q,Wang CY,Liu DY,Jian P,Qian Q,Zhou GQ and Robinson PT.2008.A brief review of ophiolites in China.Journal of Asian Earth Sciences,32(5-6):308-324
Zhong DL.1998.Paleotethysides in Western Yunnan and Sichuan,China.Beijing:Science Press,1-235(in Chinese)
Zhou DQ.2013.Deep tectonics-magmatic system and metallogenesis in the Sanjiang Tethys superimposed orogeny.Ph.D.Dissertation.Beijing:China University of Geosciences,1-141(in Chinese)
Zhu WG,Zhong H,Li XH,Deng HL,He DF,Wu KW and Bai ZJ.2013.SHRIMP zircon U-Pb geochronology,elemental,and Nd isotopic geochemistry of the Neoproterozoic mafic dykes in the Yanbian area,SW China.Precambrian Research,164(1-2):66-85
曹淑云,刘俊来,Leiss B,Vollbrecht A,邹运鑫,赵春强.2009.哀牢山-红河剪切带左行走滑作用起始时间约束---点苍山高温糜棱岩的显微构造与热年代学证据.地质学报,83(10):1388-1400
陈喜连,黄文婷,邹银桥,梁华英,张健,张玉泉.2016.玉龙斑岩铜矿带南段含矿斑岩体锆石U-Pb年龄、地球化学特征及南北段成矿规模差异分析.岩石学报,32(8):2522-2534
管涛,黄智龙,许成,张振亮,严再飞,陈觅.2006.云南白马寨镍矿区煌斑岩40Ar-39Ar定年和地球化学特征.岩石学报,22(4):873-883
郭利果,刘玉平,徐伟,张兴春,秦克章,李铁胜,石玉若.2006.SHRIMP锆石年代学对西藏玉龙斑岩铜矿成矿年龄的制约.岩石学报,22(4):1009-1016
和文言,莫宣学,喻学惠,和中华,董国臣,刘晓波,苏纲生,黄雄飞.2013.滇西北衙金多金属矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义.岩石学报,29(4):1301-1310
胡晓佳.2012.哀牢山-红河断裂带新生代富钾中酸性侵入岩的成因研究及其地质意义.硕士学位论文.西安:西北大学,1-73
靳新娣,朱和平.2000.岩石样品中43种元素的高分辨等离子质谱测定.分析化学研究简报,28(5):563-567
李宝龙,季建清,付孝悦,龚俊峰,宋彪,庆建春,张臣.2008.滇西点苍山-哀牢山变质岩系锆石SHRIMP定年及其地质意义.岩石学报,24(10):2322-2330
李宝龙,季建清,付孝悦,龚俊峰,宋彪,庆建春,张臣,马宗晋.2009.滇西点苍山-哀牢山变质岩系变质时限研究.岩石学报,25(3):595-608
李宝龙,季建清,王丹丹,马宗晋.2012.滇南新元古代的岩浆作用:来自瑶山群深变质岩SHRIMP锆石U-Pb年代学证据.地质学报,86(10):1584-1591
李龚建,王庆飞,禹丽,胡兆初,马楠,黄钰涵.2013.哀牢山古特提斯洋缝合时限:晚二叠世花岗岩类锆石U-Pb年代学与地球化学制约.岩石学报,29(11):3883-3890
刘翠,邓晋福,刘俊来,石耀霖.2011.哀牢山构造岩浆带晚二叠世-早三叠世火山岩特征及其构造环境.岩石学报,27(12):3590-3602
刘汇川,王岳军,蔡永丰,马莉燕,邢晓婉,范蔚茗.2013.哀牢山构造带新安寨晚二叠世末期过铝质花岗岩锆石U-Pb年代学及Hf同位素组成研究.大地构造与成矿学,37(1):87-98
刘汇川,王岳军,范蔚茗,Zi JW,蔡永丰,杨光林.2014.滇西哀牢山地区晚三叠世高εNd(t)-εHf(t)花岗岩的构造指示.中国科学(地球科学),44(11):2373-2388
刘俊来,宋志杰,曹淑云,翟云峰,王安建,高兰,修群业,曹殿华.2006.印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程---以藏东三江地区构造演化为例.岩石学报,22(4):775-786
刘俊来,王安建,曹淑云,邹运鑫,唐渊,陈越.2008.滇西点苍山杂岩中混合岩的地质年代学分析及其区域构造内涵.岩石学报,24(3):413-420
戚学祥,王秀华,朱路华,胡兆初,李志群.2010.滇西印支地块东北缘新元古代侵入岩形成时代的厘定及其构造意义:锆石LA-ICP-MS U-Pb定年及地球化学证据.地质学报,26(7):2141-2154
沈上越,魏启荣,程惠兰,莫宣学,冯庆来.2000.云南哀牢山带两类硅质岩特征.科学通报,45(9):988-992
田广,张长青,彭惠娟,周云满,李建荣,张星培,胡明月.2014.哀牢山长安金矿成因机制及动力学背景初探:来自LA-ICP-MS锆石U-Pb定年和黄铁矿原位微量元素测定的证据.岩石学报,30(1):125-138
王冬兵,唐渊,廖世勇,尹福光,孙志明,王立全,王保弟.2013.滇西哀牢山变质岩系锆石U-Pb定年及其地质意义.岩石学报,29(4):1261-1278
王舫,刘福来,刘平华.2011.青藏高原东南缘点苍山-哀牢山杂岩带中片麻岩的变质演化及深熔作用特征.岩石学报,27(11):3280-3294
王舫,刘福来,刘平华.2013.点苍山-哀牢山变质杂岩带变沉积岩的变质演化.岩石学报,29(2):630-640
王义昭,李兴林,段丽兰,黄志勋,崔春龙.2000.三江地区南段大地构造与成矿.北京:地质出版社,1-123
云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社,45-201
张进江,钟大赉,桑海清,周勇.2006.哀牢山-红河构造带古新世以来多期活动的构造和年代学证据.地质科学,41(2):291-310
钟大赉.1998.滇川西部古特提斯造山带.北京:科学出版社,1-235
周道卿.2013.三江特提斯复合造山带深部构造-岩浆体系与成矿作用研究.博士学位论文.北京:中国地质大学,1-141
Bureau of Geology and Mineral Resources of Yunnan Province.1990.Regional Geology of Yunnan Province.Beijing:Geological Publishing House,45-201(in Chinese)
Cai YF,Wang YJ,Cawood PA,Zhang YZ and Zhang AM.2015.Neoproterozoic crustal growth of the southern Yangtze Block:Geochemical and zircon U-Pb geochronological and Lu-Hf isotopic evidence of Neoproterozoic diorite from the Ailaoshan zone.Precambrian Research,266:137-149
Cao SY,Liu JL,Leiss B,Vollbrecht A,Zou YX and Zhao CQ.2009.Timing of initiation of left-lateral slip along the Ailao Shan-Red River shear zone:Microstructural,texture and thermochronological evidence from high temperature mylonites in Diancang Shan,SWChina.Acta Geologica Sinica,83(10):1388-1400(in Chinese with English abstract)
Cao SY,Liu JL,Leiss B,Vollbrecht A,Genser J,Neubauer F and Zhao CQ.2012.Initiation of left-lateral deformation along the Ailao ShanRed River shear zone:New microstructural,textural,and geochronological constraints from the Diancang Shan metamorphic massif,SW Yunnan,China.International Geology Review,54(3):348-367
Chen B,Long XP,Wilde SA,Yuan C,Wang Q,Xia XP and Zhang ZF.2017.Delamination of lithospheric mantle evidenced by Cenozoic potassic rocks in Yunnan,SW China:A contribution to uplift of the Eastern Tibetan Plateau.Lithos,284-285:709-729
Chen XL,Huang WT,Zou YQ,Liang HY,Zhang J and Zhang YQ.2016.Zircon U-Pb geochronology and geochemistry of ore-bearing porphyries in the southern Yulong porphyry copper belt,and factors resulting in the differences in scale of mineralization between the southern and northern Yulong porphyry copper belt.Acta Petrologica Sinica,32(8):2522-2534(in Chinese with English abstract)
Chung SL,Chu MF,Zhang YQ,Xie YW,Lo CH,Lee TY,Lan CY,Li XH,Zhang Q and Wang YZ,2005.Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism.Earth-Science Reviews,68(3-4):173-196
De la Roche H,Leterrier J,Grandclaude P and Marchal M.1980.Aclassification of volcanic and plutonic rocks using R1R2-diagram and major-element analyses:Its relationships with current nomenclature.Chemical Geology,29(1-4):183-210
Deng J,Wang QF,Li GJ and Santosh M.2014a.Cenozoic tectonomagmatic and metallogenic processes in the Sanjiang region,southwestern China.Earth-Science Reviews,138:268-299
Deng J,Wang QF,Li GJ,Li CS and Wang CM.2014b.Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region,SW China.Gondwana Research,26(2):419-437
Deng J,Wang QF,Li GJ and Zhao Y.2015.Structural control and genesis of the Oligocene Zhenyuan orogenic gold deposit,SW China.Ore Geology Reviews,65:42-54
Deng WM,Huang X and Zhong DL.1998.Petrological characteristics and genesis of Cenozoic alkali-rich porphyry in West Yunnan,China.Chinese Journal of Geology,33(4):412-425(in Chinese with English abstract)
Gao LE and Zeng LS.2014.Fluxed melting of metapelite and the formation of Miocene high-Ca O two-mica granites in the Malashan gneiss dome,southern Tibet.Geochimica et Cosmochimica Acta,130:136-155
Guan T,Huang ZL,Xu C,Zhang ZL,Yan ZF and Chen M.2006.Dating and geochemical characteristics of lamprophyres in the Baimazhai nickel deposit,Yunnan Province.Acta Petrologica Sinica,22(4):873-883(in Chinese with English abstract)
Guo LG,Liu YP,Xu W,Zhang XC,Qin KZ,Li TS and Shi YR.2006.Constraints to the mineralization age of the Yulong porphyry copper deposit from SHRIMP U-Pb zircon data in Tibet.Acta Petrologica Sinica,22(4):1009-1016(in Chinese with English abstract)
Guo ZF,Hertogen J,Liu JQ,Pasteels P,Boven A,Punzalan L,He HY,Luo XJ and Zhang WH.2005.Potassic magmatism in western Sichuan and Yunnan provinces,SE Tibet,China:Petrological and Geochemical constraints on petrogenesis.Journal of Petrology,46(1):33-78
He WY,Mo XX,Yu XH,He ZH,Dong GC,Liu XB,Su GS and Huang XF.2013.Zircon U-Pb and molybdenite Re-Os dating for the Beiya gold-polymetallic deposit in the western Yunnan Province and its geological significance.Acta Petrologica Sinica,29(4):1301-1310(in Chinese with English abstract)
Hu XJ.2012.Petrogenesis and geological significance of Cenozoic K-rich intermediate-acid plutons along Ailao Shan-Red River fault zone.Master Degree Thesis.Xi’an:Northwest University,1-73(in Chinese with English summary)
Jian P,Liu DY,Kr9ner A,Zhang Q,Wang YZ,Sun XM and Zhang W.2009.Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China(Ⅱ):Insights from zircon ages of ophiolites,arc/back-arc assemblages and within-plate igneous rocks and generation of the Emeishan CFB province.Lithos,113(3-4):767-784
Jin XD and Zhu HP.2000.Determination of 43 trace elements in rock samples by double focusing high resolution inductively coupled plasma-mass spectrometry.Chinese Journal of Analytical Chemistry,28(5):563-567(in Chinese with English abstract)
Lai CK,Meffre S,Crawford AJ,Zaw K,Xue CD and Halpin JA.2014a.The western Ailaoshan volcanic belts and their SE Asia connection:A new tectonic model for the eastern Indochina Block.Gondwana Research,26(1):52-74
Lai CK,Meffre S,Crawford AJ,Zaw K,Halpin JA,Xue CD and Salam A.2014b.The Central Ailaoshan ophiolite and modern analogs.Gondwana Research,26(1):75-88
Leloup PH,Arnaud N,Lacassin R,Kienast JR,Harrison TM,Trong TTP,Replumaz A and Tapponnier P.2001.New constraints on the structure,thermochronology,and timing of the Ailao Shan-Red River shear zone,SE Asia.Journal of Geophysical Research,106(B4):6683-6732
Li BL,Ji JQ,Fu XY,Gong JF,Song B,Qing JC and Zhang C.2008.Zircon SHRIMP dating and its geological implications of the metamorphic rocks in Ailao Shan-Diancang Mountain ranges,west Yunnan.Acta Petrologica Sinica,24(10):2322-2330(in Chinese with English abstract)
Li BL,Ji JQ,Fu XY,Gong JF,Song B,Qing JC,Zhang C and Ma ZJ.2009.Metamorphic times limits’study on the metamorphic rocks series of Ailao Shan-Diancang Mountain Ranges,West Yunnan.Acta Petrologica Sinica,25(3):595-608(in Chinese with English abstract)
Li BL,Ji JQ,Wang DD and Ma ZJ.2012.Neoproterozoic magmatism in South Yunan:Evidence from SHRIMP zircon U-Pb geochrological results of high-grade metamorphic rocks in the Yaoshan Group.Acta Geologica Sinica,86(10):1584-1591(in Chinese with English abstract)
Li GJ,Wang QF,Yu L,Hu ZC,Ma N and Huang YH.2013.Closure time of the Ailaoshan Paleo-Tethys Ocean:Constraints from the zircon U-Pb dating and geochemistry of the Late Permian granitoids.Acta Petrologica Sinica,29(11):3883-3890(in Chinese with English abstract)
Lin TH,Chung SL,Chiu HY,Wu FY,Yeh MW,Searle MP and Iizuka Y.2012.Zircon U-Pb and Hf isotope constraints from the Ailao Shan-Red River shear zone on the tectonic and crustal evolution of southwestern China.Chemical Geology,291:23-37
Liu C,Deng JF,Liu JL and Shi YL.2011.Characteristics of volcanic rocks from Late Permian to Early Triassic in Ailaoshan tectonomagmatic belt and implications for tectonic settings.Acta Petrologica Sinica,27(12):3590-3602(in Chinese with English abstract)
Liu FL,Wang F,Liu PH and Liu CH.2013.Multiple metamorphic events revealed by zircons from the Diancang Shan-Ailao Shan metamorphic complex,southeastern Tibetan Plateau.Gondwana Research,24(1):429-450
Liu FL,Wang F,Liu PH,Yang H and Meng E.2015b.Multiple partial melting events in the Ailao Shan-Red River and Gaoligong Shan complex belts,SE Tibetan Plateau:Zircon U-Pb dating of granitic leucosomes within migmatites.Journal of Asian Earth Sciences,110:151-169
Liu HC,Wang YJ,Cai YF,Ma LY,Xing XW and Fan WM.2013.Zircon U-Pb geochronology and Hf isotopic composition of the Xin’anzhai granite along the Ailaoshan tectonic zone in West Yunnan Province.Geotectonica et Metallogenia,37(1):87-98(in Chinese with English abstract)
Liu HC,Wang YJ,Fan WM,Zi JW,Cai YF and Yang GL.2014.Petrogenesis and tectonic implications of Late-Triassic highεNd(t)-εHf(t)granites in the Ailaoshan tectonic zone(SW China).Science China(Earth Sciences),57(9):2181-2194
Liu HC,Wang YJ,Cawood PA,Fan WM,Cai YF and Xing XW.2015c.Record of Tethyan ocean closure and Indosinian collision along the Ailaoshan suture zone(SW China).Gondwana Research,27(3):1292-1306
Liu JL,Song ZJ,Cao SY,Zhai YF,Wang AJ,Gao L,Xiu QY and Cao DH.2006.The dynamic setting and processes of tectonic and magmatic evolution of the oblique collision zone between Indian and Eurasian plates:Exemplified by the tectonic evolution of the Three River region,eastern Tibet.Acta Petrologica Sinica,22(4):775-786(in Chinese with English abstract)
Liu JL,Wang AJ,Cao SY,Zou YX,Tang Y and Chen Y.2008.Geochronology and tectonic implication of migmatites from Diancangshan,western Ynnnan,China.Acta Petrologica Sinica,24(3):413-420(in Chinese with English abstract)
Liu JL,Chen XY,Wu WB,Tang Y,Tran MD,Nguyen QL,Zhang ZCand Zhao ZD.2015a.New tectono-geochronological constraints on timing of shearing along the Ailao Shan-Red River shear zone:Implications for genesis of Ailao Shan gold mineralization.Journal of Asian Earth Sciences,103:70-86
Liu YS,Hu ZH,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Lu YJ,Kerrich R,Cawood PA,Mc Cuaig TC,Hart CJR,Li ZX,Hou ZQ and Bagas L.2012.Zircon SHRIMP U-Pb geochronology of potassic felsic intrusions in western Yunnan,SW China:Constraints on the relationship of magmatism to the Jinsha suture.Gondwana Research,22(2):737-747
Qi XX,Wang XH,Zhu LH,Hu ZC and Li ZQ.2010.Validation on age of Neoproterozoic intrusions from northeastern margin of Indochina block,western Yunnan and its tectonic implication:Evidence from zircon LA-ICP-MS U-Pb dating and geochemistry.Acta Petrologica Sinica,26(7):2141-2154(in Chinese with English abstract)
Qi XX,Santosh M,Zhu LH,Zhao YH,Hu ZC,Zhang C and Ji FB.2014.Mid-Neoproterozoic arc magmatism in the northeastern margin of the Indochina block,SW China:Geochronological and petrogenetic constraints and implications for Gondwana assembly.Precambrian Research,245:207-224
Qi XX,Santosh M,Zhao YH,Hu ZC,Zhang C,Ji FB and Wei C.2016.Mid-Neoproterozoic ridge subduction and magmatic evolution in the northeastern margin of the Indochina block:Evidence from geochronology and geochemistry of calc-alkaline plutons.Lithos,248-251:138-152
Searle MP.2006.Role of the Red River shear zone,Yunnan and Vietnam,in the continental extrusion of SE Asia.Journal of the Geological Society,163(6):1025-1036
Searle MP,Yeh MW,Lin TH and Chung SL.2010.Structural constraints on the timing of left-lateral shear along the Red River shear zone in the Ailao Shan and Diancang Shan Ranges,Yunnan,SW China.Geosphere,6(4):316-338
Shen SY,Wei QR,Cheng HL,Mo XX and Feng QL.2000.Two kinds of silicalites in Mount Ailao belt,Yunnan Province.Chinese Science Bulletin,45(23):2176-2180
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Tian G,Zhang CQ,Peng HJ,Zhou YM,Li JR,Zhang XP and Hu MY.2014.Petrogenesis and geodynamic setting of the Chang’an gold deposit in southern Ailaoshan metallogenic belt.Acta Petrologica Sinica,30(1):125-138(in Chinese with English abstract)
Wang DB,Tang Y,Liao SY,Yin FG,Sun ZM,Wang LQ and Wang BD.2013.Zircon U-Pb dating and its geological implications of the metamorphic rock series in Ailao Shan Ranges,western Yunnan.Acta Petrologica Sinica,29(4):1261-1278(in Chinese with English abstract)
Wang F,Liu FL and Liu PH.2011.Metamorphic evolution and anatexis of gneissic rocks in the Diancangshan-Ailaoshan metamorphic complex belt,southeastern Tibet Plateau.Acta Petrologica Sinica,27(11):3280-3294(in Chinese with English abstract)
Wang F,Liu FL and Liu PH.2013.Metamorphic evolution of metasedimentary rocks within the Diancang Shan-Ailao Shan metamorphic complex belt.Acta Petrologica Sinica,29(2):630-640(in Chinese with English abstract)
Wang F,Liu FL,Liu PH,Shi JR and Cai J.2016a.Petrology,geochemistry,and metamorphic evolution of meta-sedimentary rocks in the Diancang Shan-Ailao Shan metamorphic complex,Southeastern Tibetan Plateau.Journal of Asian Earth Sciences,124:68-93
Wang YJ,Zhou YZ,Cai YF,Liu HC,Zhang YZ and Fan WM.2016b.Geochronological and geochemical constraints on the petrogenesis of the Ailaoshan granitic and migmatite rocks and its implications on Neoproterozoic subduction along the SW Yangtze Block.Precambrian Research,283:106-124
Wang YZ,Li XL,Duan LL,Huang ZX and Cui CL.2000.Geotectonics and Metallogeny in the South Nujiang-Lancang-Jinsha Rivers Area.Beijing:Geological Publishing House,1-123(in Chinese)
Yumul GP Jr,Zhou MF,Wang CY,Zhao TP and Dimalanta CB.2008.Geology and geochemistry of the Shuanggou ophiolite(Ailao Shan ophiolitic belt),Yunnan Province,SW China:Evidence for a slowspreading oceanic basin origin.Journal of Asian Earth Sciences,32(5-6):385-395
Zeng LS,Gao LE and Xie KJ.2011.Concurrence of Mid-Miocene high Sr/Y granite and leucogranite in the Yardoi gneiss dome,Tethyan Himalaya,Southern Tibet.Mineralogical Magazine,75(3):2245
Zhang JJ,Zhong DL,Sang HQ and Zhou Y.2006.Structural and geochronological evidence for multiple episodes of deformation since Paleocene along the Ailao Shan-Red River shear zone,southeastern Asia.Chinese Journal of Geology,41(2):291-310(in Chinese with English abstract)
Zhang Q,Zhou DJ,Zhao DS,Huang ZX,Han S,Jia XQ and Dong JQ.1994.Ophiolites of the Hengduan Mountains,China:Characteristics and tectonic settings.Journal of Southeast Asian Earth Sciences,9(4):335-344
Zhang Q,Wang CY,Liu DY,Jian P,Qian Q,Zhou GQ and Robinson PT.2008.A brief review of ophiolites in China.Journal of Asian Earth Sciences,32(5-6):308-324
Zhong DL.1998.Paleotethysides in Western Yunnan and Sichuan,China.Beijing:Science Press,1-235(in Chinese)
Zhou DQ.2013.Deep tectonics-magmatic system and metallogenesis in the Sanjiang Tethys superimposed orogeny.Ph.D.Dissertation.Beijing:China University of Geosciences,1-141(in Chinese)
Zhu WG,Zhong H,Li XH,Deng HL,He DF,Wu KW and Bai ZJ.2013.SHRIMP zircon U-Pb geochronology,elemental,and Nd isotopic geochemistry of the Neoproterozoic mafic dykes in the Yanbian area,SW China.Precambrian Research,164(1-2):66-85
曹淑云,刘俊来,Leiss B,Vollbrecht A,邹运鑫,赵春强.2009.哀牢山-红河剪切带左行走滑作用起始时间约束---点苍山高温糜棱岩的显微构造与热年代学证据.地质学报,83(10):1388-1400
陈喜连,黄文婷,邹银桥,梁华英,张健,张玉泉.2016.玉龙斑岩铜矿带南段含矿斑岩体锆石U-Pb年龄、地球化学特征及南北段成矿规模差异分析.岩石学报,32(8):2522-2534
管涛,黄智龙,许成,张振亮,严再飞,陈觅.2006.云南白马寨镍矿区煌斑岩40Ar-39Ar定年和地球化学特征.岩石学报,22(4):873-883
郭利果,刘玉平,徐伟,张兴春,秦克章,李铁胜,石玉若.2006.SHRIMP锆石年代学对西藏玉龙斑岩铜矿成矿年龄的制约.岩石学报,22(4):1009-1016
和文言,莫宣学,喻学惠,和中华,董国臣,刘晓波,苏纲生,黄雄飞.2013.滇西北衙金多金属矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义.岩石学报,29(4):1301-1310
胡晓佳.2012.哀牢山-红河断裂带新生代富钾中酸性侵入岩的成因研究及其地质意义.硕士学位论文.西安:西北大学,1-73
靳新娣,朱和平.2000.岩石样品中43种元素的高分辨等离子质谱测定.分析化学研究简报,28(5):563-567
李宝龙,季建清,付孝悦,龚俊峰,宋彪,庆建春,张臣.2008.滇西点苍山-哀牢山变质岩系锆石SHRIMP定年及其地质意义.岩石学报,24(10):2322-2330
李宝龙,季建清,付孝悦,龚俊峰,宋彪,庆建春,张臣,马宗晋.2009.滇西点苍山-哀牢山变质岩系变质时限研究.岩石学报,25(3):595-608
李宝龙,季建清,王丹丹,马宗晋.2012.滇南新元古代的岩浆作用:来自瑶山群深变质岩SHRIMP锆石U-Pb年代学证据.地质学报,86(10):1584-1591
李龚建,王庆飞,禹丽,胡兆初,马楠,黄钰涵.2013.哀牢山古特提斯洋缝合时限:晚二叠世花岗岩类锆石U-Pb年代学与地球化学制约.岩石学报,29(11):3883-3890
刘翠,邓晋福,刘俊来,石耀霖.2011.哀牢山构造岩浆带晚二叠世-早三叠世火山岩特征及其构造环境.岩石学报,27(12):3590-3602
刘汇川,王岳军,蔡永丰,马莉燕,邢晓婉,范蔚茗.2013.哀牢山构造带新安寨晚二叠世末期过铝质花岗岩锆石U-Pb年代学及Hf同位素组成研究.大地构造与成矿学,37(1):87-98
刘汇川,王岳军,范蔚茗,Zi JW,蔡永丰,杨光林.2014.滇西哀牢山地区晚三叠世高εNd(t)-εHf(t)花岗岩的构造指示.中国科学(地球科学),44(11):2373-2388
刘俊来,宋志杰,曹淑云,翟云峰,王安建,高兰,修群业,曹殿华.2006.印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程---以藏东三江地区构造演化为例.岩石学报,22(4):775-786
刘俊来,王安建,曹淑云,邹运鑫,唐渊,陈越.2008.滇西点苍山杂岩中混合岩的地质年代学分析及其区域构造内涵.岩石学报,24(3):413-420
戚学祥,王秀华,朱路华,胡兆初,李志群.2010.滇西印支地块东北缘新元古代侵入岩形成时代的厘定及其构造意义:锆石LA-ICP-MS U-Pb定年及地球化学证据.地质学报,26(7):2141-2154
沈上越,魏启荣,程惠兰,莫宣学,冯庆来.2000.云南哀牢山带两类硅质岩特征.科学通报,45(9):988-992
田广,张长青,彭惠娟,周云满,李建荣,张星培,胡明月.2014.哀牢山长安金矿成因机制及动力学背景初探:来自LA-ICP-MS锆石U-Pb定年和黄铁矿原位微量元素测定的证据.岩石学报,30(1):125-138
王冬兵,唐渊,廖世勇,尹福光,孙志明,王立全,王保弟.2013.滇西哀牢山变质岩系锆石U-Pb定年及其地质意义.岩石学报,29(4):1261-1278
王舫,刘福来,刘平华.2011.青藏高原东南缘点苍山-哀牢山杂岩带中片麻岩的变质演化及深熔作用特征.岩石学报,27(11):3280-3294
王舫,刘福来,刘平华.2013.点苍山-哀牢山变质杂岩带变沉积岩的变质演化.岩石学报,29(2):630-640
王义昭,李兴林,段丽兰,黄志勋,崔春龙.2000.三江地区南段大地构造与成矿.北京:地质出版社,1-123
云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社,45-201
张进江,钟大赉,桑海清,周勇.2006.哀牢山-红河构造带古新世以来多期活动的构造和年代学证据.地质科学,41(2):291-310
钟大赉.1998.滇川西部古特提斯造山带.北京:科学出版社,1-235
周道卿.2013.三江特提斯复合造山带深部构造-岩浆体系与成矿作用研究.博士学位论文.北京:中国地质大学,1-141