南秦岭佛坪隆起的构造过程及成因机制
|
摘要
佛坪隆起位于东、西秦岭交接的最狭窄部位,北邻商丹缝合带,南接勉略缝合带,属南秦岭构造带(秦岭微板块),也是华北板块和扬子板块挤压作用最为强烈的地区之一。该区以前寒武纪变质基底的穹状出露和印支期花岗岩的广泛侵入为主要地质特征,区内岩石组合可划分为结晶基底、过渡基底、外围盖层岩系及中酸性侵入岩体,古老的基底主要出露于佛坪县城及其北侧的龙草坪一带。佛坪隆起遭受了多期次、多层次的构造变形作用的改造,主要表现为早期以基底为主的塑性变形及晚期的脆-韧性变形。该区现今的主体构造主要表现为一系列东西向展布的褶皱构造,反映了强烈的南北向挤压作用。县城隆起和龙草坪隆起位于两个背斜的核部。
佛坪地区的变质特征显示,以佛坪隆起核部为核心,麻粒岩相-高角闪岩相-低角闪岩相-高绿片岩相-低绿片岩相变质带呈同心环状向外展布的空间分布规律。其变质条带的这种同心环状展布,也揭示了其“穹窿”构造特征。其中麻粒岩主要出露于佛坪县城南约500m河东岸,呈条带状和透镜状产出,其矿物组成以透辉石、斜长石、角闪石、黑云母及石榴子石为主。该区混合岩化作用发育,根据其产出特征和构造形态认为其成因系深部岩浆作用所致。
本文在对佛坪隆起基底及其周围地区构造面理和线理的系统测量和统计的基础上,通过古应力场恢复,进而揭示区域构造应力场分布规律,探讨佛坪隆起的形成机制。研究结果表明,佛坪隆起的主体及其北部龙草坪隆起区外围地层中的构造片理呈外倾的封闭环状展布,在平面上呈东-西长、南-北短的椭圆形,揭示了县城隆起和龙草坪隆起总体具有“改造穹窿”的构造特征,而这种改造来自于印支期的近南-北向挤压构造体制。
根据该区构造形迹特征,对其产状进行测量和统计,并判断其运动学指向,从而恢复隆起区古构造应力场。古应力场分析表明,县城隆起及龙草坪隆起区的两期构造具有类似的分布规律和特点：第一期构造最大主应力(σ1)呈以隆起核部为核心的高角度外倾,最小主应力(σ3)则表现为近于水平放射状展布；第二期构造最大主应力(σ1)总体呈现近水平的南-北或北东-南西向展布,最小主应力(σ3)多为东-向或北西-南东向伸展。揭示了县城隆起与龙草坪隆起具有相同或类似的成因机制和构造演化过程。隆起区主要遭受两期构造变形的叠加改造,即早期垂向隆升和后期南-北挤压作用。第一期构造是由于扬子板块向北俯冲,导致岛弧区在主体挤压作用下叠加深部岩浆上涌,使得岛弧基底发生穹状隆升,佛坪基底抬升主要生成于这种穹状隆起,它与该区岩浆侵入活动密切相关；第二期构造是由于扬子板块和秦岭微板块沿勉略带的碰撞造山作用,使得原岛弧区遭受近南北向挤压,形成近东西向的构造形迹,并叠加改造了先期穹隆构造的位态。佛坪穹隆是在早期深部岩浆作用下发生近垂直的穹状隆升,并叠加了后期南北向挤压构造才奠定了其基本构造面貌。
该区岩浆岩中锆石U-Pb定年结果为212±1.5Ma,代表了岩浆岩主体结晶时代,稍晚于秦岭造山带主碰撞期,其成因可能为秦岭造山期后的下地壳拆沉作用。测得混合岩中变质锆石的U-Pb年龄为182.3±1.1Ma,代表了一期由部分熔融作用导致的混合岩化作用,表明秦岭造山带已经发生构造体制转换,进入伸展构造阶段。由于燕山期秦岭造山带受到巴山弧形逆冲推覆构造及汉南地块向北东向挤入,处于秦岭造山最狭窄地带的佛坪地区遭受最强烈的挤压作用,并持续隆升,并进一步剥露地表。
Foping dome, which located in the junction of Eastern and Western Qinling, is belongs to South Qinling tectonic belts (Qinling micro-plate). This dome sites between Shangxian-Danfeng suture zone and Mianxian-Lueyang suture zone, and it is also one of the strongest compression areas by North China Block and Yangtze Block. Foping area is characterized by outcropping of Precambrian metamorphic basement and Indosinian granite. The rock assemblage in this area can be classified into crystalline basement, translation basement, caprock rocks, and intermediate-acid intrusive rocks. The crystalline basement mainly outcrops at Foping town and Longcaoping. It suffered multi-period and multilevel deformation in Foping area, and the structural characteristics here show a series of fold structure, which spreads nearly east-west and reflects a strong north-south compression. The Foping town dome and Longcaoping dome locate at the nuclear of two anticlines.
The metamorphism in Foping area shows:the granulite facie-High-amphibolite facies-Low-amphibolite facie-High-greenschist facie-Low-greenschist facie spread in the shape of concentric rings and to the core of Foping dome in the plane, which can also proves the "Dome" structure features. The granulite facie rock shows lenticulars, mainly outcrops at about 500 meters to the town, east of river. The major minerals of these rocks are diopside, plagioclase, hornblende, biotite and garnet. The migmatization developed well in this region, which maybe caused by deep magmatism.
The study of paleostress fields by systematic measurement and statistics on the tectonic foliation and lineation in the Foping dome and its adjacent areas. This can reveal the distribution of regional paleostress fields, by which we can discuss the genetic mechanism of the Foping dome. The results show that the foliation in Foping and Longcaoping uplifting and their adjacent stratum proves the circle features with outward trend, and longer in E-W, shorter in S-N in the plane. It proves that the view Foping uplifting is a thermal dome, which is transformed by latter tectonic, that is the nearly N-S compression tectonic in Indosian.
The recovery of the paleostress field is based on systematic measurement of the occurrences and the judge of the kinematic meaning in the field. The characteristics of the paleostress fields in Foping County and it northern Longcaoping revealed that the similar paleostress fields. The first phase structure shows:the compression stress (al) generally proves outward trend with high angles, with the core of the core of the domes, and the tensile stress (σ3) generally proves nearly horizontal radial spreading. The second phase structure shows:the compression stress (σ1) generally spread nearly horizontal, N-S or NE-SW, and the tensile stress (σ3) generally mainly proves extension with E-W or NW-NE. It reveals that the town uplifting and Longcaoping uplifting shared the same of similar genetic mechanism and tectonic evolution. The uplifting area suffers two stages'deformations, which are vertical uplifting in the early stage and N-S compression in the latter stage.
The first stage structure was caused by the northward subduction of Yangtze Plate. The uplifting of the basement of Foping dome was closely related with the deep magmatism and granite intrusion, which was generated by the subduction. The second stage structure was caused by the collision orogeny between Yangtze Block and Qinling Micro-Plate, which leaded the N-S compression in the island-arc zone, and it superposited on the early structures and formed a series E-W structures. The combination of regional tectonic interpretation and the analysis of principal stress field demonstrate that Foping dome underwent a sub-vertical uplifting period, which was superimposed by the latter tectonic of the N-S compressive.
The result of U-Pb zircon dating shows that the main magmatic crystallization is 212±1.5Ma, which is later on the time of main orogenic period. The magma intrusion may be a result of delamination. We also get the dating 182.3±1.1Ma from the migmatites in this region, it reveals a migmatization in this period. The result proves that the structural transformation had occurred in Qinling belt and had been in the extensional tectonic stage. In Yanshania, because of the NE direction compression of Bashan arc thrust structure, Foping area, which sited the most narrow zone of Qinling orogeny, suffered the most intense compression. The Foping dome continued uplifting and was further exhumated to the surface.
佛坪地区的变质特征显示,以佛坪隆起核部为核心,麻粒岩相-高角闪岩相-低角闪岩相-高绿片岩相-低绿片岩相变质带呈同心环状向外展布的空间分布规律。其变质条带的这种同心环状展布,也揭示了其“穹窿”构造特征。其中麻粒岩主要出露于佛坪县城南约500m河东岸,呈条带状和透镜状产出,其矿物组成以透辉石、斜长石、角闪石、黑云母及石榴子石为主。该区混合岩化作用发育,根据其产出特征和构造形态认为其成因系深部岩浆作用所致。
本文在对佛坪隆起基底及其周围地区构造面理和线理的系统测量和统计的基础上,通过古应力场恢复,进而揭示区域构造应力场分布规律,探讨佛坪隆起的形成机制。研究结果表明,佛坪隆起的主体及其北部龙草坪隆起区外围地层中的构造片理呈外倾的封闭环状展布,在平面上呈东-西长、南-北短的椭圆形,揭示了县城隆起和龙草坪隆起总体具有“改造穹窿”的构造特征,而这种改造来自于印支期的近南-北向挤压构造体制。
根据该区构造形迹特征,对其产状进行测量和统计,并判断其运动学指向,从而恢复隆起区古构造应力场。古应力场分析表明,县城隆起及龙草坪隆起区的两期构造具有类似的分布规律和特点：第一期构造最大主应力(σ1)呈以隆起核部为核心的高角度外倾,最小主应力(σ3)则表现为近于水平放射状展布；第二期构造最大主应力(σ1)总体呈现近水平的南-北或北东-南西向展布,最小主应力(σ3)多为东-向或北西-南东向伸展。揭示了县城隆起与龙草坪隆起具有相同或类似的成因机制和构造演化过程。隆起区主要遭受两期构造变形的叠加改造,即早期垂向隆升和后期南-北挤压作用。第一期构造是由于扬子板块向北俯冲,导致岛弧区在主体挤压作用下叠加深部岩浆上涌,使得岛弧基底发生穹状隆升,佛坪基底抬升主要生成于这种穹状隆起,它与该区岩浆侵入活动密切相关；第二期构造是由于扬子板块和秦岭微板块沿勉略带的碰撞造山作用,使得原岛弧区遭受近南北向挤压,形成近东西向的构造形迹,并叠加改造了先期穹隆构造的位态。佛坪穹隆是在早期深部岩浆作用下发生近垂直的穹状隆升,并叠加了后期南北向挤压构造才奠定了其基本构造面貌。
该区岩浆岩中锆石U-Pb定年结果为212±1.5Ma,代表了岩浆岩主体结晶时代,稍晚于秦岭造山带主碰撞期,其成因可能为秦岭造山期后的下地壳拆沉作用。测得混合岩中变质锆石的U-Pb年龄为182.3±1.1Ma,代表了一期由部分熔融作用导致的混合岩化作用,表明秦岭造山带已经发生构造体制转换,进入伸展构造阶段。由于燕山期秦岭造山带受到巴山弧形逆冲推覆构造及汉南地块向北东向挤入,处于秦岭造山最狭窄地带的佛坪地区遭受最强烈的挤压作用,并持续隆升,并进一步剥露地表。
Foping dome, which located in the junction of Eastern and Western Qinling, is belongs to South Qinling tectonic belts (Qinling micro-plate). This dome sites between Shangxian-Danfeng suture zone and Mianxian-Lueyang suture zone, and it is also one of the strongest compression areas by North China Block and Yangtze Block. Foping area is characterized by outcropping of Precambrian metamorphic basement and Indosinian granite. The rock assemblage in this area can be classified into crystalline basement, translation basement, caprock rocks, and intermediate-acid intrusive rocks. The crystalline basement mainly outcrops at Foping town and Longcaoping. It suffered multi-period and multilevel deformation in Foping area, and the structural characteristics here show a series of fold structure, which spreads nearly east-west and reflects a strong north-south compression. The Foping town dome and Longcaoping dome locate at the nuclear of two anticlines.
The metamorphism in Foping area shows:the granulite facie-High-amphibolite facies-Low-amphibolite facie-High-greenschist facie-Low-greenschist facie spread in the shape of concentric rings and to the core of Foping dome in the plane, which can also proves the "Dome" structure features. The granulite facie rock shows lenticulars, mainly outcrops at about 500 meters to the town, east of river. The major minerals of these rocks are diopside, plagioclase, hornblende, biotite and garnet. The migmatization developed well in this region, which maybe caused by deep magmatism.
The study of paleostress fields by systematic measurement and statistics on the tectonic foliation and lineation in the Foping dome and its adjacent areas. This can reveal the distribution of regional paleostress fields, by which we can discuss the genetic mechanism of the Foping dome. The results show that the foliation in Foping and Longcaoping uplifting and their adjacent stratum proves the circle features with outward trend, and longer in E-W, shorter in S-N in the plane. It proves that the view Foping uplifting is a thermal dome, which is transformed by latter tectonic, that is the nearly N-S compression tectonic in Indosian.
The recovery of the paleostress field is based on systematic measurement of the occurrences and the judge of the kinematic meaning in the field. The characteristics of the paleostress fields in Foping County and it northern Longcaoping revealed that the similar paleostress fields. The first phase structure shows:the compression stress (al) generally proves outward trend with high angles, with the core of the core of the domes, and the tensile stress (σ3) generally proves nearly horizontal radial spreading. The second phase structure shows:the compression stress (σ1) generally spread nearly horizontal, N-S or NE-SW, and the tensile stress (σ3) generally mainly proves extension with E-W or NW-NE. It reveals that the town uplifting and Longcaoping uplifting shared the same of similar genetic mechanism and tectonic evolution. The uplifting area suffers two stages'deformations, which are vertical uplifting in the early stage and N-S compression in the latter stage.
The first stage structure was caused by the northward subduction of Yangtze Plate. The uplifting of the basement of Foping dome was closely related with the deep magmatism and granite intrusion, which was generated by the subduction. The second stage structure was caused by the collision orogeny between Yangtze Block and Qinling Micro-Plate, which leaded the N-S compression in the island-arc zone, and it superposited on the early structures and formed a series E-W structures. The combination of regional tectonic interpretation and the analysis of principal stress field demonstrate that Foping dome underwent a sub-vertical uplifting period, which was superimposed by the latter tectonic of the N-S compressive.
The result of U-Pb zircon dating shows that the main magmatic crystallization is 212±1.5Ma, which is later on the time of main orogenic period. The magma intrusion may be a result of delamination. We also get the dating 182.3±1.1Ma from the migmatites in this region, it reveals a migmatization in this period. The result proves that the structural transformation had occurred in Qinling belt and had been in the extensional tectonic stage. In Yanshania, because of the NE direction compression of Bashan arc thrust structure, Foping area, which sited the most narrow zone of Qinling orogeny, suffered the most intense compression. The Foping dome continued uplifting and was further exhumated to the surface.
引文
常宏,王向利,能伟.1998.南秦岭佛坪穹窿基底组成[J].西北地质,19(3)：6-11
程裕淇.1987.有关混合岩和混合岩化作用的一些问题——对半个世纪以来某些基本认识的回顾[J].中国地质科学院院报,第16号：5-19
陈陇刚,代新宇,李宁等.1999.佛坪地区中元古代孔慈岩系地质特征[J].西安工程学院学报,21(2)：19-23
代新宁.1997.佛坪地区元古界火山岩的厘定[J].陕西地矿信息,22(34)：6-9
董云鹏,张国伟,赖绍聪等.1999.随州花山蛇绿构造混杂岩的厘定及其大地构造意义[J].中国科学(D辑),29(3)：222-231
董云鹏,查显峰,付明庆等.2008.秦岭南缘大巴山褶皱-冲断推覆构造的特征[J].地质通报,27(9)：1493-1595
董云鹏,周鼎武,张国伟等.1998.秦岭造山带南缘早古生代基性火山岩地球化学特征及其大地构造意义[J].地球化学,27(5)：432-441
董云鹏,张国伟,朱炳泉.2003.北秦岭构造属性与元古代构造演化[J].地球学报,24(1)：3-10
管树巍,李本亮,何登发等.2007.复杂构造解析中的几何学方法与应用[J].地质科学,42(2)：722-739
韩郁菁.1999.变质作用p-T-t轨迹[M].北京：中国地质大学出版社
何建坤,卢华夏,朱斌.1999.东秦岭造山带南缘北大巴山构造反转及其动力学[J].SCIENTIAGEOLOGICA SINICA.34(2):139-153
贺同兴.1987.混合岩化作用的地质成因分类[J].中国地质科学院院报,第16号：95-98
侯治华,钟南才,侯逾昆等.2006.辽宁浑河断裂带及其临近地区水系格局构造节理与构造应力场的研究[J].防灾科技学院学报,8(4)：6-10
胡建民,孟庆任,白武明等.2002.南秦岭构造带中-晚古生代伸展构造作用[J].地质通报,21(8-9)：471-477
赖绍聪,秦江峰.2009.南秦岭勉略缝合带蛇绿岩与火山岩[M].北京：科学出版社
赖绍聪,张国伟,董云鹏等.2003.秦岭-大别勉略构造带蛇绿岩与相关火山岩性质及时空分布[J].中国科学(D辑),33(12)：1174-1183
李海平.1998.陕西省佛坪发现太古宇结晶杂岩[J].中国区域地质,17(3)：329-330
李锦轶,王宗起,赵民.1999.秦岭山脉南部略阳碰撞造山作用时代的40Ar／39Ar年代学证据[J].地质学报(英文版),73(2)：189-190
李曙光,侯振辉,杨永成等.2003.南秦岭勉略构造带三岔子古岩浆弧的地球化学特征及形成时代[J]. 中国科学(D辑),33(12)：1163-1173
刘树根,李智武,刘顺等.2006.大巴山前陆盆地——神断带的形成演化[M].北京：地质出版社
刘和甫.1995.伸展构造及其反转作用[J].地学前缘(中国地质大学,北京),2(1-2)：113-124
陆松年.1995.大陆地壳演化时间维的确定及存在问题[J].新疆地质,13(1)：13-19
罗照华,莫宣学,万渝生等.2006.青藏高原最年轻碱性玄武岩SHRIMP年龄的地质意义[J].岩石学报,22(3)：578-584
李亚林,王根宝,王成善等.2000.南秦岭龙草坪结晶杂岩锆石U-Pb同位素地质年代学研究[J].矿物学报,20(1)：50-54
李亚林,张国伟,王成善等.2001.秦岭免略缝合带两期韧性剪切变形及其动力学意义[J].成都理工学院学报,28(1)：28-33
李岩峰,曲国胜,刘殊等.2008.米仓山、南大巴山前缘构造特征及其形成机制[J].大地构造与成矿学,32(3)：285-292
陆松年,陈志宏,李怀坤等.秦岭造山带中两条新元古代岩浆岩带[J].地质学报,2005,79(2)：165-173
马文璞主编.1992.区域构造解析——方法理论和中国板块构造[J].地质出版社：54-61
盘晓东,康力.2002.浑江断裂带及水系的分形特征和构造活动性研究[J].东北地震研究,18(4)：7-15
丘元禧.2000.论构造筛分[J].地质力学学报,6(1)：33-43
陕西省地质调查院.2004.《汉中市幅》1：25万地质图(I48C 003004)及说明书,《镇安县幅》1：25万地质图(149C 003001)及说明书[R]
陕西省地质矿产局.1989.陕西省区域地质志[R].中华人民共和国地质矿产部,地质专报(一)区域地质.北京：地质出版社,第13号
邵克忠译.1963.变质岩矿物和构造演变[M].北京：中国工业出版社.29-50
宋传中.2000.秦岭-大别山北部后造山期构造格架与形成机制[J].合肥工业大学学报(自然科学版),23(2)：221-226
孙延贵,张国伟,国安林等.2004.秦-昆联结构造及其构造过程的同位素年代学证据[J].中国地质,31(4)：372-378
索书田.1987.构造解析(下册)[M].武汉地质学院区地教研室,32-144
王非,朱日祥,李齐等.2004.秦岭造山带的差异隆升特征——花岗岩40Ar／39Ar年代学研究的证据[J].地学前缘,11(4)：445-459
王根宝.1997.南秦岭佛坪片麻岩系同位素年代学及其地质意义[J].西北地质科学,18(2)：21-25
王根宝.1997.佛坪穹窿有新说[J].陕西地质,15(2)
王根宝,李三忠.1998.论秦岭佛坪地区隆-滑构造[J].长春科技大学学报,28(1)：23-29
王娟,李鑫,赖绍聪等.2008.印支期南秦岭西茬河、五龙岩体成因及构造意义[J].中国地质,35(2)：207-216
王居里.1995.秦岭造山带佛坪地区花岗岩类的特征及其意义[J].西北大学学报(自然科学版),25(5)：497-502
王居里.1997.佛坪地区印支期花岗岩的成因[J].西北大学学报(自然科学版),27(6)：521-524
王居里.1997.秦岭造山带佛坪隆起的变质作用、岩浆活动及其构造演化[D].西安：西北大学
王居里,张国伟.1999.秦岭佛坪穹窿盖层岩系的地质和地球化学特征[J].西北大学学报(自然科学版),29(5)：417-421
王居里.2002.秦岭造山带佛坪基底杂岩的地质特征[J].西北地质,35(2)：1-8
王涛.2000.花岗岩研究与大陆动力学[J].地学前缘(中国地质大学,北京),第7卷增刊,137-145
魏春景,张翠光.2002.陆-陆碰撞造山带中压型变质作用的pT轨迹——以南秦岭佛坪地区为例[J].岩石矿物学杂志,21(4)：356-362
魏春景,杨崇辉,张寿广.1998.南秦岭造山带东段的变质作用及其地质意义[J].地质学报(英文版)论文摘要,73(1)：93-94
魏宽义.2003.构造解析学[M].陕西人民教育出版社
吴峰辉,刘树文,李秋根等.2009.西秦岭光头山花岗岩U-Pb年代学及其地质意义[J].北京大学学报(自然科学版)网络版,第1期2009-03-30
武汉地质学院区地教研室著.1987.地质构造形迹图册[M].地质出版社.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,49(16)：1589-1604
吴元保,唐俊,张少兵等.2007.北大别两期混合岩化作用：SHRIMP锆石U-Pb年龄证据[J].科学通报,52(8)：939-944
夏林沂.2001.造山带火山岩浆作用[J].西北地质,34(3)：18-28
徐学义,何世平,王洪亮等.2008.中国西北部地质概论[M].北京：科学出版社
徐继峰,韩吟文.1996.秦岭古MORB型岩石的高放射成因铅同位素组成——特提斯型古洋幔存在的证据[J].中国科学(D辑),26(增刊)：34-41
许志琴,张建新,徐惠芬等.1997.中国主要大陆山链韧性剪切及动力学[M].北京：地质出版社
杨崇辉,魏春景,张寿广等.1999.南秦岭佛坪地区麻粒岩相岩石锆石U-Pb年龄[J].地质论评,45(2)：173-179
杨经绥,刘来福,吴才来等.2003.中央碰撞造山带中两期超高压变质作用：来自含柯石英锆石的定年证据[J].地质学报,77(4)：464-478
杨经绥,许志琴,裴先治等.2002.秦岭发现金刚石：横贯中国中部巨型超高压变质带新证据及古生代和中生代两期深俯冲作用的识别[J].地质学报,76(4)：484-495
杨巍然,游振东.1995.秦岭-大别高压超高压变质带构造特征及构造演化[J].高校地质学报,1(2)：53-64
杨钊.2008.南秦岭中断中-新元古代基底火山岩地球化学特征及其构造意义[D].西安：西北大学
游振东,索书田,韩郁菁等.1991.造山带核部杂岩变质过程与构造解析——以东秦岭为例[M].地质矿产部秦巴重点攻关科研项目.北京：中国地质大学出版社
袁洪林,吴福元,高山等.2003.东北地区新生代侵入岩的激光锆石探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,48(4)：1511-1520
翟刚毅.2000.东秦岭佛坪穹隆变质作用与构造动力学分析[J].矿物岩石,20(6)：86-90
张本仁,高山,张宏飞等.2002.秦岭造山带地球化学[M].北京：科学出版社
张寿广,魏春昱,杨崇辉.1998.南秦岭造山带东段的变质作用研究[J].地学前缘,5(4)：210
张寿广,魏春景,赵子然等.1996.东秦岭陡岭杂岩的形成与变质演化[J].中国科学(D辑),第26卷增刊：73-77
张国伟,陈家义主编.1996.秦岭造山带大地构造图.北京：科学出版社,1996年6月第一次印刷
张国伟,孟庆任,赖绍聪.1995.秦岭造山带的结构构造[J].中国科学(B辑),25(9)：994-1003
张国伟,孟庆任,于在平等.1996.秦岭造山带的造山过程及其动力学特征[J].中国科学(D辑),26(3)：193-200
张国伟,张本仁,袁学诚等.1988.秦岭造山带的形成及其演化[M].西安：西北大学出版社
张国伟,张本仁,袁学诚等.2001.秦岭造山带与大陆动力学[M].北京：科学出版社
张升全,张飚.1997.佛坪地区片麻岩套地质特征[J].陕西地质,15(2)：15-20
张岳桥,施炜,廖昌珍等.2006.鄂尔多斯盆地周边断裂运动学分析与晚中生代构造应力场体制转换[J].地质学报,80(5)：639-647
张宗清,宋彪,唐索寒等.2004.秦岭佛坪变质结晶岩系年龄和物质组成特征——SHRIMP锆英石U-Pb年代学和全岩Sm-Nd年代学数据[J].中国地质,31(2)：161-168
张宗清,张国伟,唐索寒等.汉南侵入杂岩年龄及其快速冷凝原因[J].科学通报,2000,45(23)：2567-2572
赵凤清,赵文平,左义成等.2006.陕西汉中地区新元古代岩浆岩U-Pb年代学[J].地质通报,25(3)：383-388
赵玉灵,杨金中,沈远超.2002.同位素地质学定年方法评述[J].地质勘探,第2期63-69
邹付戈,尹宏伟.2009.四川龙门山地区反转构造样式分析及其成因机制探讨[J].大地构造与成矿学.33(3)：321-333
朱铭.1995.秦岭地区花岗岩的K-Ar等时线年龄和39Ar-40Ar年龄及其地质意义[J].岩石学报,11(2)：179-182
朱志澄主编.1999.构造地质学[M].中国地质大学出版社
Axel Gerdes, Aemin Zeh.2009. Zircon formation versus zircon alteration-New insights from combined U-Pb and Lu-Hf in-situ LA-ICP-MS analyses, and consequences for the interpretation of Archean ziron from the Central Zone of the Limpopo Belt[J]. Chemical Geology,261:230-241
Axel K. Schmitt, Daniel F. Stochli, Brian P. Hausback.2006. Eruption and magma crystallization age of Las Tres virgenes (BaJa California) constrained by combined 230Th/238U and (U-Th)/He dating of zircon[J]. Journal of Volcanology and Geothermal Research,158:281-295
Baldwin S. and Maher W.1997. Spatial and Temporal Variation of Selenium Concentration in Five Species of Intertidal Molluscs from Jervis Bay, Australia[J]. Marin Environmental Research,44(3),243-262.
Baldwin S. L., Fitzgerald P.G. 2006. Using thermochronology to determine the timing and rates of tectonic processes[J]. Goldschmidt Conference Abstracts, A32.
Bjorn S. Hardarson & J. Godfrey Fitton.1991. Increased mantle melting beneath Snaefellsjokull wolcano during Late Pleistocene deglaciation[J]. NATURE,353(5):62-64
Bradley R. Hacher, Lathar Ratschbacher, Laura Webb, Trevor Ireland, et al.1998. U/Pb zircon ages constrain the architecture of the Ultrahigh-pressure Qinling-Dabie Orogen, China[J]. Earth and Planetary Science Letters,161:215-230
Cheng Shunyou,Zhang Guowei,Diao Bo,et al.2007. A preliminary study on the Lithospheric thermal-rheological structure of the East Qinling orogenic belt[J]. Front. Earth Sci. China, 1(1):116-120
Dirk Frei, Axel Gerdes.2009. Precise and accurate in situ U-Pb dating of zircon with high sample throughput by automated LA-SF-MS[J]. Chemical Geology,261:261-270
Dong Yun-Peng, Zhou Mei-Fu, Zhang Guo-Wei, et al.2008. The Grenvillian Songshugou ophiolite in the Qinling Mountains, Central China:Implications for the tectonic evolution of the Qinling orogenic belt[J]. Journal of Asian Earth Sciences,32:325-335
Fitzgerald P.G., Baldwin S.L., Webb L.E. et al.2006. Interpretation of (U-Th)/He single grain ages from slowly cooled crustal terranes:A case study from the Transantarctic Mountains of Southern Victoria Land[J]. Chemical Geology,225,91-120.
HAN Yigui, ZHANG Shihong, Franco PIRAJNO.2007. Evolution of the Mesozoic Granites in the Xiong'ershan-Waifangshan Region,Western Henan Province, China, and Its Tectonic Implications[J]. Acta Geologica Sinica,81(2):253-265
Harrison T M.1981. Diffusion of 40Ar in hornblende[J]. Contribution to Mineralogy and Petrology,78, 324-331.
John G. Ramsay, Martin I. Huber.1983. The Techniques of Modern Structural Geology, Volume 1:strain analysis[M].
K. M. Goodenough, R.J. Thomas, B. De Waele, R. M. Key, D.I. Schofield, W.Bauer, et al.2009. Post-collisional magmatism in the central East African Orogen:The Maevarano Suite of north Madagascar[J]. LITHOS, ACCEPTED MANUSCRIPT.
Lothar Ratschbacher, Bradley R. Hacker, Andrew Calvert et.al.2003. Tectonics of the Qinling (central China):tectonostratigraphy, geochronology, and deformation history[J]. Tectonophysics,366:1-53
Meng Qing-Ren, Wang Erchie, Hu Jian-Min.2005. Mesozoic sedimentary evolution of the northwest Sichuan basin:Implication for continued clockwise rotation of the South China Block[J]. Geological Society of America Bulletin, March/April,396-410
Meng Qingren, Zhang Guowei.2000. Geologic framework and tectonic evolution of the Qinling Orogen, central China[J]. Tectonophysics,323:183-196
Mihai N. Ducea, Jibamitra Ganguly, Erin J. Rosenberg, et al.2003. Sm-Nd dating of Spatially controlled domains of garnet single crystals:a new method of high-temperature thermochronology[J]. Earth and Planetary Science Letters,213,31-42.
Nicolas Bellahsen, Patricia Fiore, David D. Pollard.2006. The role of fractures in the structural interpretation of the Sheep Mountain Anticline, Wyoming [J]. Journal of Geology,28:850-867
Peter W. Reiners and Kenneth A. Farley.1999. Helium diffusion and (U-Th)/He themochronometry of titanite[J]. Geochimica et Cosmochimica Acta, Vol.63,No.22,pp.3845-3859.
Peter W. Reiners, Kenneth A. Farley.2001. Influence of crystal size on apatite (U-Th)/He thermochronology:an example from the Bighorn Mountains, Wyoming[J]. Earth and Planetary Science Letters,188,423-420.
Peter W. Reiners, Terry L. Spell, Stefan Nicolescu et al.2004. Zircon (U-Th)/He thermochronometry:He diffusion and comparisons with 40Ar/39Ar dating[J]. Geochimica et Cosmochimica Acta, Vol.68, No.8, pp.1857-1887.
Ren Jianye,Li Sitian,et al.1998. Extensional Tectonic System of Erlian Fault Basin Group and Its Deep Background[J]. Jaurnal of China University of Geosciences,9(3):230-235
Rey P, Vanderhaeghe O, Teyssier C. Gravitational collapse of the continental crust:Eefinition, regimes and modes[J]. Tectonophysics,2001,342:435-449
Scott Johnston, George Gehrels, Wictor Valenvia, Joaquin Ruiz.2009. Small-volume U-Pb zircon geochronology by laser ablation-multicollector-ICP-MS[J].Chemical Geology 259:218-229
Sun W D, Li S G, Chen Y D, et al.2002. Timing of synorogic granotids in the south Qinling Dbie Orogenic Belt[J]. Geology,110:457-468
SUN Yangui, Chen Zhengxing, Liu Yong'an.2000. Junction and Evolution of the Qinling, Qilian and Kunlun Orogenic Belts[J]. Acta Geologica Sinica,74(2):223-228
Whitney D. L, Teyssier C, Fayon A K, et al.2003. Tectonic controls on metamorphism, partial melting, and intrusion:Timing and duration of regional metamorphism and magmatism in the Nigde Massif, Turkey[J]. Tectonophysics,376:37-60
Wu Yuan-Bao, John M. Hanchar, Gao Shan, et al.2009. Age and nature of eclogites in the Huwan shear zone, and the multi-stage evolution of the Qinling-Dabie-Sulu orogen, central China[J]. Earth and Planetary Science Letters,345-354
Xu Ji-feng, Zhang Ben-ren, Han Yin-wen.2008. Geochemistry of the Mian-Lue ophiolites in the Qinling Moutains, central China:Constraints on the evolution of the Qinling orogenic belt and collision of the North and south China Cratons[J]. Journal of Asian Earth Sciences,32:336-347
ZHANG Chengli, LI Miao, WANG Tao, al.2004. U-Pb Zircon Geochronology and Geochenmistry of Granitoids in the Douling Group in the Eastern Qinling[J]. ACTA GEOLOGICA SINICA,78(1):83-95
Zhang Chengli, Zhou Dingwu.1999. Rifting of Wudang Block During Chenjiang Period of Neoproterozoic in South Qinling of China:Geochemical Evidence from Wudang Basic Byke Swarm[J]. Gondwana Research,2 (4):529-532
Zhang Yue Qiao, Pierre Vergely, Jacques Mercier.1995. Active faulting in and along the Qinling Range (China) inferred from Spot imagery analysis and extrusion tectonics of south China[J]. Tectonophysics, 243:69-95
程裕淇.1987.有关混合岩和混合岩化作用的一些问题——对半个世纪以来某些基本认识的回顾[J].中国地质科学院院报,第16号：5-19
陈陇刚,代新宇,李宁等.1999.佛坪地区中元古代孔慈岩系地质特征[J].西安工程学院学报,21(2)：19-23
代新宁.1997.佛坪地区元古界火山岩的厘定[J].陕西地矿信息,22(34)：6-9
董云鹏,张国伟,赖绍聪等.1999.随州花山蛇绿构造混杂岩的厘定及其大地构造意义[J].中国科学(D辑),29(3)：222-231
董云鹏,查显峰,付明庆等.2008.秦岭南缘大巴山褶皱-冲断推覆构造的特征[J].地质通报,27(9)：1493-1595
董云鹏,周鼎武,张国伟等.1998.秦岭造山带南缘早古生代基性火山岩地球化学特征及其大地构造意义[J].地球化学,27(5)：432-441
董云鹏,张国伟,朱炳泉.2003.北秦岭构造属性与元古代构造演化[J].地球学报,24(1)：3-10
管树巍,李本亮,何登发等.2007.复杂构造解析中的几何学方法与应用[J].地质科学,42(2)：722-739
韩郁菁.1999.变质作用p-T-t轨迹[M].北京：中国地质大学出版社
何建坤,卢华夏,朱斌.1999.东秦岭造山带南缘北大巴山构造反转及其动力学[J].SCIENTIAGEOLOGICA SINICA.34(2):139-153
贺同兴.1987.混合岩化作用的地质成因分类[J].中国地质科学院院报,第16号：95-98
侯治华,钟南才,侯逾昆等.2006.辽宁浑河断裂带及其临近地区水系格局构造节理与构造应力场的研究[J].防灾科技学院学报,8(4)：6-10
胡建民,孟庆任,白武明等.2002.南秦岭构造带中-晚古生代伸展构造作用[J].地质通报,21(8-9)：471-477
赖绍聪,秦江峰.2009.南秦岭勉略缝合带蛇绿岩与火山岩[M].北京：科学出版社
赖绍聪,张国伟,董云鹏等.2003.秦岭-大别勉略构造带蛇绿岩与相关火山岩性质及时空分布[J].中国科学(D辑),33(12)：1174-1183
李海平.1998.陕西省佛坪发现太古宇结晶杂岩[J].中国区域地质,17(3)：329-330
李锦轶,王宗起,赵民.1999.秦岭山脉南部略阳碰撞造山作用时代的40Ar／39Ar年代学证据[J].地质学报(英文版),73(2)：189-190
李曙光,侯振辉,杨永成等.2003.南秦岭勉略构造带三岔子古岩浆弧的地球化学特征及形成时代[J]. 中国科学(D辑),33(12)：1163-1173
刘树根,李智武,刘顺等.2006.大巴山前陆盆地——神断带的形成演化[M].北京：地质出版社
刘和甫.1995.伸展构造及其反转作用[J].地学前缘(中国地质大学,北京),2(1-2)：113-124
陆松年.1995.大陆地壳演化时间维的确定及存在问题[J].新疆地质,13(1)：13-19
罗照华,莫宣学,万渝生等.2006.青藏高原最年轻碱性玄武岩SHRIMP年龄的地质意义[J].岩石学报,22(3)：578-584
李亚林,王根宝,王成善等.2000.南秦岭龙草坪结晶杂岩锆石U-Pb同位素地质年代学研究[J].矿物学报,20(1)：50-54
李亚林,张国伟,王成善等.2001.秦岭免略缝合带两期韧性剪切变形及其动力学意义[J].成都理工学院学报,28(1)：28-33
李岩峰,曲国胜,刘殊等.2008.米仓山、南大巴山前缘构造特征及其形成机制[J].大地构造与成矿学,32(3)：285-292
陆松年,陈志宏,李怀坤等.秦岭造山带中两条新元古代岩浆岩带[J].地质学报,2005,79(2)：165-173
马文璞主编.1992.区域构造解析——方法理论和中国板块构造[J].地质出版社：54-61
盘晓东,康力.2002.浑江断裂带及水系的分形特征和构造活动性研究[J].东北地震研究,18(4)：7-15
丘元禧.2000.论构造筛分[J].地质力学学报,6(1)：33-43
陕西省地质调查院.2004.《汉中市幅》1：25万地质图(I48C 003004)及说明书,《镇安县幅》1：25万地质图(149C 003001)及说明书[R]
陕西省地质矿产局.1989.陕西省区域地质志[R].中华人民共和国地质矿产部,地质专报(一)区域地质.北京：地质出版社,第13号
邵克忠译.1963.变质岩矿物和构造演变[M].北京：中国工业出版社.29-50
宋传中.2000.秦岭-大别山北部后造山期构造格架与形成机制[J].合肥工业大学学报(自然科学版),23(2)：221-226
孙延贵,张国伟,国安林等.2004.秦-昆联结构造及其构造过程的同位素年代学证据[J].中国地质,31(4)：372-378
索书田.1987.构造解析(下册)[M].武汉地质学院区地教研室,32-144
王非,朱日祥,李齐等.2004.秦岭造山带的差异隆升特征——花岗岩40Ar／39Ar年代学研究的证据[J].地学前缘,11(4)：445-459
王根宝.1997.南秦岭佛坪片麻岩系同位素年代学及其地质意义[J].西北地质科学,18(2)：21-25
王根宝.1997.佛坪穹窿有新说[J].陕西地质,15(2)
王根宝,李三忠.1998.论秦岭佛坪地区隆-滑构造[J].长春科技大学学报,28(1)：23-29
王娟,李鑫,赖绍聪等.2008.印支期南秦岭西茬河、五龙岩体成因及构造意义[J].中国地质,35(2)：207-216
王居里.1995.秦岭造山带佛坪地区花岗岩类的特征及其意义[J].西北大学学报(自然科学版),25(5)：497-502
王居里.1997.佛坪地区印支期花岗岩的成因[J].西北大学学报(自然科学版),27(6)：521-524
王居里.1997.秦岭造山带佛坪隆起的变质作用、岩浆活动及其构造演化[D].西安：西北大学
王居里,张国伟.1999.秦岭佛坪穹窿盖层岩系的地质和地球化学特征[J].西北大学学报(自然科学版),29(5)：417-421
王居里.2002.秦岭造山带佛坪基底杂岩的地质特征[J].西北地质,35(2)：1-8
王涛.2000.花岗岩研究与大陆动力学[J].地学前缘(中国地质大学,北京),第7卷增刊,137-145
魏春景,张翠光.2002.陆-陆碰撞造山带中压型变质作用的pT轨迹——以南秦岭佛坪地区为例[J].岩石矿物学杂志,21(4)：356-362
魏春景,杨崇辉,张寿广.1998.南秦岭造山带东段的变质作用及其地质意义[J].地质学报(英文版)论文摘要,73(1)：93-94
魏宽义.2003.构造解析学[M].陕西人民教育出版社
吴峰辉,刘树文,李秋根等.2009.西秦岭光头山花岗岩U-Pb年代学及其地质意义[J].北京大学学报(自然科学版)网络版,第1期2009-03-30
武汉地质学院区地教研室著.1987.地质构造形迹图册[M].地质出版社.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,49(16)：1589-1604
吴元保,唐俊,张少兵等.2007.北大别两期混合岩化作用：SHRIMP锆石U-Pb年龄证据[J].科学通报,52(8)：939-944
夏林沂.2001.造山带火山岩浆作用[J].西北地质,34(3)：18-28
徐学义,何世平,王洪亮等.2008.中国西北部地质概论[M].北京：科学出版社
徐继峰,韩吟文.1996.秦岭古MORB型岩石的高放射成因铅同位素组成——特提斯型古洋幔存在的证据[J].中国科学(D辑),26(增刊)：34-41
许志琴,张建新,徐惠芬等.1997.中国主要大陆山链韧性剪切及动力学[M].北京：地质出版社
杨崇辉,魏春景,张寿广等.1999.南秦岭佛坪地区麻粒岩相岩石锆石U-Pb年龄[J].地质论评,45(2)：173-179
杨经绥,刘来福,吴才来等.2003.中央碰撞造山带中两期超高压变质作用：来自含柯石英锆石的定年证据[J].地质学报,77(4)：464-478
杨经绥,许志琴,裴先治等.2002.秦岭发现金刚石：横贯中国中部巨型超高压变质带新证据及古生代和中生代两期深俯冲作用的识别[J].地质学报,76(4)：484-495
杨巍然,游振东.1995.秦岭-大别高压超高压变质带构造特征及构造演化[J].高校地质学报,1(2)：53-64
杨钊.2008.南秦岭中断中-新元古代基底火山岩地球化学特征及其构造意义[D].西安：西北大学
游振东,索书田,韩郁菁等.1991.造山带核部杂岩变质过程与构造解析——以东秦岭为例[M].地质矿产部秦巴重点攻关科研项目.北京：中国地质大学出版社
袁洪林,吴福元,高山等.2003.东北地区新生代侵入岩的激光锆石探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,48(4)：1511-1520
翟刚毅.2000.东秦岭佛坪穹隆变质作用与构造动力学分析[J].矿物岩石,20(6)：86-90
张本仁,高山,张宏飞等.2002.秦岭造山带地球化学[M].北京：科学出版社
张寿广,魏春昱,杨崇辉.1998.南秦岭造山带东段的变质作用研究[J].地学前缘,5(4)：210
张寿广,魏春景,赵子然等.1996.东秦岭陡岭杂岩的形成与变质演化[J].中国科学(D辑),第26卷增刊：73-77
张国伟,陈家义主编.1996.秦岭造山带大地构造图.北京：科学出版社,1996年6月第一次印刷
张国伟,孟庆任,赖绍聪.1995.秦岭造山带的结构构造[J].中国科学(B辑),25(9)：994-1003
张国伟,孟庆任,于在平等.1996.秦岭造山带的造山过程及其动力学特征[J].中国科学(D辑),26(3)：193-200
张国伟,张本仁,袁学诚等.1988.秦岭造山带的形成及其演化[M].西安：西北大学出版社
张国伟,张本仁,袁学诚等.2001.秦岭造山带与大陆动力学[M].北京：科学出版社
张升全,张飚.1997.佛坪地区片麻岩套地质特征[J].陕西地质,15(2)：15-20
张岳桥,施炜,廖昌珍等.2006.鄂尔多斯盆地周边断裂运动学分析与晚中生代构造应力场体制转换[J].地质学报,80(5)：639-647
张宗清,宋彪,唐索寒等.2004.秦岭佛坪变质结晶岩系年龄和物质组成特征——SHRIMP锆英石U-Pb年代学和全岩Sm-Nd年代学数据[J].中国地质,31(2)：161-168
张宗清,张国伟,唐索寒等.汉南侵入杂岩年龄及其快速冷凝原因[J].科学通报,2000,45(23)：2567-2572
赵凤清,赵文平,左义成等.2006.陕西汉中地区新元古代岩浆岩U-Pb年代学[J].地质通报,25(3)：383-388
赵玉灵,杨金中,沈远超.2002.同位素地质学定年方法评述[J].地质勘探,第2期63-69
邹付戈,尹宏伟.2009.四川龙门山地区反转构造样式分析及其成因机制探讨[J].大地构造与成矿学.33(3)：321-333
朱铭.1995.秦岭地区花岗岩的K-Ar等时线年龄和39Ar-40Ar年龄及其地质意义[J].岩石学报,11(2)：179-182
朱志澄主编.1999.构造地质学[M].中国地质大学出版社
Axel Gerdes, Aemin Zeh.2009. Zircon formation versus zircon alteration-New insights from combined U-Pb and Lu-Hf in-situ LA-ICP-MS analyses, and consequences for the interpretation of Archean ziron from the Central Zone of the Limpopo Belt[J]. Chemical Geology,261:230-241
Axel K. Schmitt, Daniel F. Stochli, Brian P. Hausback.2006. Eruption and magma crystallization age of Las Tres virgenes (BaJa California) constrained by combined 230Th/238U and (U-Th)/He dating of zircon[J]. Journal of Volcanology and Geothermal Research,158:281-295
Baldwin S. and Maher W.1997. Spatial and Temporal Variation of Selenium Concentration in Five Species of Intertidal Molluscs from Jervis Bay, Australia[J]. Marin Environmental Research,44(3),243-262.
Baldwin S. L., Fitzgerald P.G. 2006. Using thermochronology to determine the timing and rates of tectonic processes[J]. Goldschmidt Conference Abstracts, A32.
Bjorn S. Hardarson & J. Godfrey Fitton.1991. Increased mantle melting beneath Snaefellsjokull wolcano during Late Pleistocene deglaciation[J]. NATURE,353(5):62-64
Bradley R. Hacher, Lathar Ratschbacher, Laura Webb, Trevor Ireland, et al.1998. U/Pb zircon ages constrain the architecture of the Ultrahigh-pressure Qinling-Dabie Orogen, China[J]. Earth and Planetary Science Letters,161:215-230
Cheng Shunyou,Zhang Guowei,Diao Bo,et al.2007. A preliminary study on the Lithospheric thermal-rheological structure of the East Qinling orogenic belt[J]. Front. Earth Sci. China, 1(1):116-120
Dirk Frei, Axel Gerdes.2009. Precise and accurate in situ U-Pb dating of zircon with high sample throughput by automated LA-SF-MS[J]. Chemical Geology,261:261-270
Dong Yun-Peng, Zhou Mei-Fu, Zhang Guo-Wei, et al.2008. The Grenvillian Songshugou ophiolite in the Qinling Mountains, Central China:Implications for the tectonic evolution of the Qinling orogenic belt[J]. Journal of Asian Earth Sciences,32:325-335
Fitzgerald P.G., Baldwin S.L., Webb L.E. et al.2006. Interpretation of (U-Th)/He single grain ages from slowly cooled crustal terranes:A case study from the Transantarctic Mountains of Southern Victoria Land[J]. Chemical Geology,225,91-120.
HAN Yigui, ZHANG Shihong, Franco PIRAJNO.2007. Evolution of the Mesozoic Granites in the Xiong'ershan-Waifangshan Region,Western Henan Province, China, and Its Tectonic Implications[J]. Acta Geologica Sinica,81(2):253-265
Harrison T M.1981. Diffusion of 40Ar in hornblende[J]. Contribution to Mineralogy and Petrology,78, 324-331.
John G. Ramsay, Martin I. Huber.1983. The Techniques of Modern Structural Geology, Volume 1:strain analysis[M].
K. M. Goodenough, R.J. Thomas, B. De Waele, R. M. Key, D.I. Schofield, W.Bauer, et al.2009. Post-collisional magmatism in the central East African Orogen:The Maevarano Suite of north Madagascar[J]. LITHOS, ACCEPTED MANUSCRIPT.
Lothar Ratschbacher, Bradley R. Hacker, Andrew Calvert et.al.2003. Tectonics of the Qinling (central China):tectonostratigraphy, geochronology, and deformation history[J]. Tectonophysics,366:1-53
Meng Qing-Ren, Wang Erchie, Hu Jian-Min.2005. Mesozoic sedimentary evolution of the northwest Sichuan basin:Implication for continued clockwise rotation of the South China Block[J]. Geological Society of America Bulletin, March/April,396-410
Meng Qingren, Zhang Guowei.2000. Geologic framework and tectonic evolution of the Qinling Orogen, central China[J]. Tectonophysics,323:183-196
Mihai N. Ducea, Jibamitra Ganguly, Erin J. Rosenberg, et al.2003. Sm-Nd dating of Spatially controlled domains of garnet single crystals:a new method of high-temperature thermochronology[J]. Earth and Planetary Science Letters,213,31-42.
Nicolas Bellahsen, Patricia Fiore, David D. Pollard.2006. The role of fractures in the structural interpretation of the Sheep Mountain Anticline, Wyoming [J]. Journal of Geology,28:850-867
Peter W. Reiners and Kenneth A. Farley.1999. Helium diffusion and (U-Th)/He themochronometry of titanite[J]. Geochimica et Cosmochimica Acta, Vol.63,No.22,pp.3845-3859.
Peter W. Reiners, Kenneth A. Farley.2001. Influence of crystal size on apatite (U-Th)/He thermochronology:an example from the Bighorn Mountains, Wyoming[J]. Earth and Planetary Science Letters,188,423-420.
Peter W. Reiners, Terry L. Spell, Stefan Nicolescu et al.2004. Zircon (U-Th)/He thermochronometry:He diffusion and comparisons with 40Ar/39Ar dating[J]. Geochimica et Cosmochimica Acta, Vol.68, No.8, pp.1857-1887.
Ren Jianye,Li Sitian,et al.1998. Extensional Tectonic System of Erlian Fault Basin Group and Its Deep Background[J]. Jaurnal of China University of Geosciences,9(3):230-235
Rey P, Vanderhaeghe O, Teyssier C. Gravitational collapse of the continental crust:Eefinition, regimes and modes[J]. Tectonophysics,2001,342:435-449
Scott Johnston, George Gehrels, Wictor Valenvia, Joaquin Ruiz.2009. Small-volume U-Pb zircon geochronology by laser ablation-multicollector-ICP-MS[J].Chemical Geology 259:218-229
Sun W D, Li S G, Chen Y D, et al.2002. Timing of synorogic granotids in the south Qinling Dbie Orogenic Belt[J]. Geology,110:457-468
SUN Yangui, Chen Zhengxing, Liu Yong'an.2000. Junction and Evolution of the Qinling, Qilian and Kunlun Orogenic Belts[J]. Acta Geologica Sinica,74(2):223-228
Whitney D. L, Teyssier C, Fayon A K, et al.2003. Tectonic controls on metamorphism, partial melting, and intrusion:Timing and duration of regional metamorphism and magmatism in the Nigde Massif, Turkey[J]. Tectonophysics,376:37-60
Wu Yuan-Bao, John M. Hanchar, Gao Shan, et al.2009. Age and nature of eclogites in the Huwan shear zone, and the multi-stage evolution of the Qinling-Dabie-Sulu orogen, central China[J]. Earth and Planetary Science Letters,345-354
Xu Ji-feng, Zhang Ben-ren, Han Yin-wen.2008. Geochemistry of the Mian-Lue ophiolites in the Qinling Moutains, central China:Constraints on the evolution of the Qinling orogenic belt and collision of the North and south China Cratons[J]. Journal of Asian Earth Sciences,32:336-347
ZHANG Chengli, LI Miao, WANG Tao, al.2004. U-Pb Zircon Geochronology and Geochenmistry of Granitoids in the Douling Group in the Eastern Qinling[J]. ACTA GEOLOGICA SINICA,78(1):83-95
Zhang Chengli, Zhou Dingwu.1999. Rifting of Wudang Block During Chenjiang Period of Neoproterozoic in South Qinling of China:Geochemical Evidence from Wudang Basic Byke Swarm[J]. Gondwana Research,2 (4):529-532
Zhang Yue Qiao, Pierre Vergely, Jacques Mercier.1995. Active faulting in and along the Qinling Range (China) inferred from Spot imagery analysis and extrusion tectonics of south China[J]. Tectonophysics, 243:69-95