缅甸中央盆地北部新生代隆升的裂变径迹证据
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摘要
缅甸中央盆地北部新生代隆升作用的研究,不仅对全面认识西缅地块的演化具有重要的意义,而且对该地区的油气勘探也具有重要的指导意义.对采自研究区的2个碎屑岩样、1个钻井基底样品进行了磷灰石裂变径迹测年及热历史模拟分析.在弧前钦敦坳陷西缘冲断带、东缘冲起带和西缅岛弧带获得了逐渐变年轻的裂变径迹年龄(分别是70.6±9.3Ma、53.4±7.5Ma和22.7±3.0Ma),表明缅甸中央盆地北部在空间上存在自西向东的递进变形过程.磷灰石的热历史模拟分析显示,缅甸中央盆地北部自晚白垩世(80±1Ma)开始,经历了隆升→快速隆升→平稳→缓慢隆升4个阶段.缅甸中央盆地29~20Ma的快速隆升冷却事件是缅甸北部区域性隆升剥露作用的体现;4Ma以来缅甸中央盆地缓慢隆升,这一构造事件是印度板块向东挤压碰撞作用的响应.研究表明缅甸中央沉积盆地的空间发育演化与递进式构造变形(隆升)是新特提斯洋/印度洋岩石圈在新生代期间向西缅地块下的多期次俯冲的直接响应.
Study of the Cenozoic uplift of the northern Central Myanmar basin is crucial to better understand both the evolution of the West Burma block and the petroleum exploration in this area.Apatite fission track dating and thermal history modeling were carried out on two detrital samples and one core bedrock sample in this study.Our results show decreasing apatite fission track(AFT)ages in western thrust belt and eastern margin of the Chindwin subbasin to the magmatic arc belt of Myanmar(i.e.,70.6±9.3 Ma,53.4±7.5 Ma and 22.7±3.0 Ma),indicating aprogressive deformation of the northern Central Myanmar basin from west to east.Furthermore,the thermal modeling results indicate that in the Late Cretaceous(80±1 Ma)uplift process of the northern Central Myanmar basin can be divided into four stages:uplifting,rapid uplifting,steady uplifting,and slow uplifting.The rapid uplift and cooling event at the 29-20 Ma represents the regional uplift and exhumation in the northern Central Myanmar basin,followed by the slow uplift of the basin since 4 Ma,which is interpreted as the result of eastward movement and intense collision of the Indian plate with respect to the Asian plate.Our study suggests that the Cenozoic development and progressive deformation of the northern Central Myanmar basin was the direct result of multi-phase subduction of the Neo-Tethyan/Indian lithosphere to the West Burma block.
Study of the Cenozoic uplift of the northern Central Myanmar basin is crucial to better understand both the evolution of the West Burma block and the petroleum exploration in this area.Apatite fission track dating and thermal history modeling were carried out on two detrital samples and one core bedrock sample in this study.Our results show decreasing apatite fission track(AFT)ages in western thrust belt and eastern margin of the Chindwin subbasin to the magmatic arc belt of Myanmar(i.e.,70.6±9.3 Ma,53.4±7.5 Ma and 22.7±3.0 Ma),indicating aprogressive deformation of the northern Central Myanmar basin from west to east.Furthermore,the thermal modeling results indicate that in the Late Cretaceous(80±1 Ma)uplift process of the northern Central Myanmar basin can be divided into four stages:uplifting,rapid uplifting,steady uplifting,and slow uplifting.The rapid uplift and cooling event at the 29-20 Ma represents the regional uplift and exhumation in the northern Central Myanmar basin,followed by the slow uplift of the basin since 4 Ma,which is interpreted as the result of eastward movement and intense collision of the Indian plate with respect to the Asian plate.Our study suggests that the Cenozoic development and progressive deformation of the northern Central Myanmar basin was the direct result of multi-phase subduction of the Neo-Tethyan/Indian lithosphere to the West Burma block.
引文
Acharyya,S.K.,2007.Collisional Emplacement History of the Naga-Andaman Ophiolites and the Position of the Eastern Indian Suture.Journal of Asian Earth Science,29(2-3):229-242.https://doi.org/10.1016/j.jseaes.2006.03.003
Allen,R.,Najman,Y.,Carter,A.,et al.,2008.Provenance of the Tertiary Sedimentary Rocks of the Indo-Burman Ranges,Burma(Myanmar):Burman Arc or Himalayan-Derived?Journal of the Geological Society,165(6):1045-1057.https://doi.org/10.1144/0016-76492007-143
Barber,A.J.,Crow,M.J.,2009.Structure of Sumatra and Its Implications for the Tectonic Assembly of Southeast Asia and the Destruction of Paleotethys.Island Arc,18(1):3-20.https://doi.org/10.1111/j.1440-1738.2008.00631.x
Barber,A.J.,Crow,M.J.,de Smet,M.E.M.,2005.Chapter14:Tectonic Evolution.In:Barber,A.J.,Crow,M.J.,Milsom,J.S.,eds.,Sumatra:Geology,Resources and Tectonic Evolution.Geological Society,London,Memoir,31:234-259.https://doi.org/10.1144/GSL.MEM.2005.031.01.14
Bender,F.,1983.Geology of Burma.Borntraeger,Berlin,293.
Bertrand,G.,Rangin,C.,2003.Tectonics of the Western Margin of the Shan Plateau(Central Myanmar):Implication for the India-Indochina Oblique Convergence since the Oligocene.Journal of Asian Earth Sciences,21(10):1139-1157.https://doi.org/10.1016/s1367-9120(02)00183-9
Bertrand,G.,Rangin,C.,Maluski,H.,et al.,2001.Diachronous Cooling along the Mogok Metamorphic Belt(Shan Scarp,Myanmar):The Trace of the Northward Migration of the Indian Syntaxis.Journal of Asian Earth Sciences,19(5):649-659.https://doi.org/10.1016/s1367-9120(00)00061-4
Chen,H.H.,Zhu,X.M.,Huang,H.D.,et al.,2017.Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis.Earth Science,42(11):1955-1971(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.124
Curray,J.R.,2005.Tectonics History of the Andaman Sea Region.Journal of Asian Earth Sciences,25(1):187-232.https://doi.org/10.1016/j.jseaes.2004.09.001
Curray,J.R.,Moore,D.G.,Lawver,L.A.,et al.,1979.Tectonics of the Andaman Sea and Burma.In:Watkins,J.,Montadert,L.,Dickinson,P.,eds.,Geological and Geophysical Investigation of Continental Slopes and Rises.American Association of Petroleum Geologists Memoir,29:189-198.
Donelick,R.A.,Ketcham,R.A.,Carlson,W.D.,1999.Variability of Apatite Fission-Track Annealing Kinetics:II.Crystallographic Orientation Effects.American Mineralogist,84(9):1224-1234.https://doi.org/10.2138/am-1999-0902
Donelick,R.A.,O’Sullivan,P.B.,Ketcham,R.A.,et al.,2005.Apatite Fission-Track Analysis.Reviews in Mineralogy and Geochemistry,58(1):49-94.https://doi.org/10.2138/rmg.2005.58.3
Gallagher,K.,Brown,R.,Johnson,C.,1998.Fission Track Analysis and Its Applications to Geological Problems.Annual Reviews of Earth and Planetary Science,26(1):519-572.https://doi.org/10.1146/annurev.earth.26.1.519
Jaeger,J.J.,Soe,A.N.,Chavasseau,O.,et al.,2011.First Hominoid from the Late Miocene of the Irrawaddy Formation(Myanmar).Plos One,6(4):e17065.https://doi.org/10.1371/journal.pone.0017065
Ketcham,R.A.,2005.Forward and Inverse Modeling of LowTemperature Thermochronometry Data.Reviews in Mineralogy and Geochemistry,58(1):275-314.https://doi.org/10.2138/rmg.2005.58.11
Ketcham,R.A.,Donelick,R.A.,Balestrieri,M.L.,et al.,2009.Reproducibility of Apatite Fission-Track Length Data and Thermal History Reconstruction.Earth and Planetary Science Letters,284(3-4):504-515.https://doi.org/10.1016/j.tifl.2009.05.015
Ketcham,R.A.,Donelick,R.A.,Carlson,W.D.,1999.Variability of Apatite Fission-Track Annealing Kinetics;III,Extrapolation to Geological Time Scales.American Mineralogist,84(9):1235-1255.https://doi.org/10.2138/am-1999-0903
Laslett,G.M.,Green,P.F.,Duddy,I.R.,et al.,1987.Thermal Annealing of Fission Tracks in Apatite 2.A Quantitative Analysis.Chemical Geology:Isotope Geoscience Section,65(1):1-13.https://doi.org/10.1016/0168-9622(87)90057-1
Li,R.Y.,Mei,L.F.,Zhu,G.H.,et al.,2013.Late Mesozoic to Cenozoic Tectonic Events in Volcanic Arc,West Burma Block:Evidences from U-Pb Zircon Dating and Apatite Fission Track Data of Granitoids.Journal of Earth Science,24(4):553-568.https://doi.org/10.1007/s12583-013-0349-7
Licht,A.,France-Lanord,C.,Reisberg,L.,et al.,2013.APalaeo Tibet-Myanmar Connection?Reconstructing the Late Eocene Drainage System of Central Myanmar Using a Multi-Proxy Approach.Journal of the Geological Society,170(6):929-939.https://doi.org/10.1144/jgs2012-126
Licht,A.,Reisberg,L.,France-Lanord,C.,et al.,2015.Cenozoic Evolution of the Central Myanmar Drainage System:Insights from Sediment Provenance in the Minbu Sub-Basin.Basin Research,28(2):237-251.https://doi.org/10.13039/501100003135
Maurin,T.,Rangin,C.,2009.Structure and Kinematics of the Indo-Burmese Wedge:Recent and Fast Growth of the Outer Wedge.Tectonics,28(2):TC2010.https://doi.org/10.1029/2008tc002276
Metcalfe,I.,2011.Tectonic Framework and Phanerozoic Evolution of Sundaland.Gondwana Research,19(1):3-21.https://doi.org/10.1016/j.gr.2010.02.016
Metcalfe,I.,2013.Gondwana Dispersion and Asian Accretion:Tectonic and Palaeogeographic Evolution of Eastern Tethys.Journal of Asian Earth Sciences,66:1-33.https://doi.org/10.1016/j.jseaes.2012.12.020
Mitchell,A.,Chung,S.L.,Oo,T.,et al.,2012.Zircon U-Pb Ages in Myanmar:Magmatic-Metamorphic Events and the Closure of a Neo-Tethys Ocean?Journal of Asian Earth Sciences,56:1-23.https://doi.org/10.1016/j.jseaes.2012.04.019
Mitchell,A.H.G.,1993.Cretaceous-Cenozoic Tectonic Events in the Western Myanmar(Burma)-Assam Region.Journal of the Geological Society,150(6):1089-1102.https://doi.org/10.1144/gsjgs.150.6.1089
Naing,T.T.,Bussien,D.A.,Winkler,W.H.,et al.,2013.Provenance Study on Eocene-Miocene Sandstones of the Rakhine Coastal Belt,Indo-Burman Ranges of Myanmar:Geodynamic Implications.Geological Society,London,Special Publications,386(1):195-216.https://doi.org/10.1144/SP386.10
Nielsen,C.,Chamot-Rooke,N.,Rangin,C.,2004.From Partial to Full Strain Partitioning along the Indo-Burmese Hyper-Oblique Subduction.Marine Geology,209(1-4):303-327.https://doi.org/10.1016/j.margeo.2004.05.001
Oo,K.L.,Zaw,K.,Meffre,S.,et al.,2015.Provenance of the Eocene Sandstones in the Southern Chindwin Basin,Myanmar:Implications for the Unroofing History of the Cretaceous-Eocene Magmatic Arc.Journal of Asian Earth Sciences,107:172-194.https://doi.org/10.1016/j.jseaes.2015.04.029
Pal,T.,Chakraborty,P.P.,Gupta,T.D.,et al.,2003.Geodynamic Evolution of the Outer-Arc-Forearc Belt in the Andaman Islands,the Central Part of the Burma-Java Subduction Complex.Geological Magazine,140(3):289-307.https://doi.org/10.1017/S0016756803007805
Pivnik,D.A.,Nahm,J.,Tucker,S.,et al.,1998.Polyphase Deformation in a Fore-Arc/Back-Arc Basin,Salin Subbasin,Myanmar(Burma).American Association of Petroleum Geologists Bulletin,82:1837-1856.https://doi.org/10.1306/1d9bd15f-172d-11d7-8645000102c1865d
Searle,M.P.,Noble,S.R.,Cottle,J.M.,et al.,2007.Tectonic Evolution of the Mogok Metamorphic Belt,Burma(Myanmar)Constrained by U-Th-Pb Dating of Metamorphic and Magmatic Rocks.Tectonics,26(3):TC3014.https://doi.org/10.1029/2006tc002083
Shen,C.B.,Mei,L.F.,Liu,Z.Q.,et al.,2009.Apatite and Zircon Fission Track Data,Evidences for the MesozoicCenozoic Uplift of Huangling Dome,Central China.Journal of Mineralogy and Petrology,29(2):45-60(in Chinese with English abstract).
Wandrey,C.J.,2006.Eocene to Miocene Composite Total Petroleum System,Irrawaddy-Andaman and North Burma Geologic Provinces,Myanmar,Chapter E.In:Wandrey,C.J.,ed.,Petroleum Systems and Related Geologic Studies in Region 8,South Asia.Geological Survey Bulletin,2208:26.
Wang,J.G.,Wu,F.Y.,Tan,X.C.,et al.,2014.Magmatic Evolution of the Western Myanmar Arc Documented by U-Pb and Hf Isotopes in Detrital Zircon.Tectonophysics,612-613:97-105.https://doi.org/10.1016/j.tecto.2013.11.03
Xie,N.,Jiang,Y.,Zhu,G.H.,et al.,2010.Evolution of the Sagaing Strike-Slip Fault and Its Control of Shuibo Basin Structural Evolution,Myanmar.Geoscience,24(2):268-272(in Chinese with English abstract).
Zhang,P.,Mei,L.F.,Ma,Y.X.,et al.,2014.Tectonic Features and Dynamic Evolution of Bay of Bengal Basin:New Insights into Satellite-Gravity and Seismic Data.Earth Science,39(10):1307-1321(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2014.123
Zhang,P.,Mei,L.F.,Hu,X.L.,et al.,2017a.Structures,Uplift,and Magmatism of the Western Myanmar Arc:Constraints to Mid-Cretaceous-Paleogene Tectonic Evolution of the Western Myanmar Continental Margin.Gondwana Research,52:18-38.https://doi.org/10.1016/j.gr.2017.09.002
Zhang,P.,Mei,L.F.,Xiong,P.,et al.,2017b.Structural Features and Proto-Type Basin Reconstructions of the Bay of Bengal Basin:A Remnant Ocean Basin Model.Journal of Earth Science,28(4):666-682.https://doi.org/10.1007/s12583-017-0750-8
陈贺贺,朱筱敏,黄捍东,等,2017.基于碎屑锆石定年的饶阳凹陷蠡县斜坡沙河街组物源分析.地球科学,42(11):1955-1971.https://doi.org/10.3799/dqkx.2017.124
沈传波,梅廉夫,刘昭茜,等,2009.黄陵隆起中-新生代隆升作用的裂变径迹证据.矿物岩石,29(2):45-60.
谢楠,姜烨,朱光辉,等,2010.缅甸Sagaing走滑断裂及对睡宝盆地构造演化的控制和影响.现代地质,24(2):268-272.
张朋,梅廉夫,马一行,等,2014.孟加拉湾盆地构造特征与动力学演化:来自卫星重力与地震资料的新认识.地球科学,39(10):1307-1321.https://doi.org/10.3799/dqkx.2014.123
Allen,R.,Najman,Y.,Carter,A.,et al.,2008.Provenance of the Tertiary Sedimentary Rocks of the Indo-Burman Ranges,Burma(Myanmar):Burman Arc or Himalayan-Derived?Journal of the Geological Society,165(6):1045-1057.https://doi.org/10.1144/0016-76492007-143
Barber,A.J.,Crow,M.J.,2009.Structure of Sumatra and Its Implications for the Tectonic Assembly of Southeast Asia and the Destruction of Paleotethys.Island Arc,18(1):3-20.https://doi.org/10.1111/j.1440-1738.2008.00631.x
Barber,A.J.,Crow,M.J.,de Smet,M.E.M.,2005.Chapter14:Tectonic Evolution.In:Barber,A.J.,Crow,M.J.,Milsom,J.S.,eds.,Sumatra:Geology,Resources and Tectonic Evolution.Geological Society,London,Memoir,31:234-259.https://doi.org/10.1144/GSL.MEM.2005.031.01.14
Bender,F.,1983.Geology of Burma.Borntraeger,Berlin,293.
Bertrand,G.,Rangin,C.,2003.Tectonics of the Western Margin of the Shan Plateau(Central Myanmar):Implication for the India-Indochina Oblique Convergence since the Oligocene.Journal of Asian Earth Sciences,21(10):1139-1157.https://doi.org/10.1016/s1367-9120(02)00183-9
Bertrand,G.,Rangin,C.,Maluski,H.,et al.,2001.Diachronous Cooling along the Mogok Metamorphic Belt(Shan Scarp,Myanmar):The Trace of the Northward Migration of the Indian Syntaxis.Journal of Asian Earth Sciences,19(5):649-659.https://doi.org/10.1016/s1367-9120(00)00061-4
Chen,H.H.,Zhu,X.M.,Huang,H.D.,et al.,2017.Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis.Earth Science,42(11):1955-1971(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.124
Curray,J.R.,2005.Tectonics History of the Andaman Sea Region.Journal of Asian Earth Sciences,25(1):187-232.https://doi.org/10.1016/j.jseaes.2004.09.001
Curray,J.R.,Moore,D.G.,Lawver,L.A.,et al.,1979.Tectonics of the Andaman Sea and Burma.In:Watkins,J.,Montadert,L.,Dickinson,P.,eds.,Geological and Geophysical Investigation of Continental Slopes and Rises.American Association of Petroleum Geologists Memoir,29:189-198.
Donelick,R.A.,Ketcham,R.A.,Carlson,W.D.,1999.Variability of Apatite Fission-Track Annealing Kinetics:II.Crystallographic Orientation Effects.American Mineralogist,84(9):1224-1234.https://doi.org/10.2138/am-1999-0902
Donelick,R.A.,O’Sullivan,P.B.,Ketcham,R.A.,et al.,2005.Apatite Fission-Track Analysis.Reviews in Mineralogy and Geochemistry,58(1):49-94.https://doi.org/10.2138/rmg.2005.58.3
Gallagher,K.,Brown,R.,Johnson,C.,1998.Fission Track Analysis and Its Applications to Geological Problems.Annual Reviews of Earth and Planetary Science,26(1):519-572.https://doi.org/10.1146/annurev.earth.26.1.519
Jaeger,J.J.,Soe,A.N.,Chavasseau,O.,et al.,2011.First Hominoid from the Late Miocene of the Irrawaddy Formation(Myanmar).Plos One,6(4):e17065.https://doi.org/10.1371/journal.pone.0017065
Ketcham,R.A.,2005.Forward and Inverse Modeling of LowTemperature Thermochronometry Data.Reviews in Mineralogy and Geochemistry,58(1):275-314.https://doi.org/10.2138/rmg.2005.58.11
Ketcham,R.A.,Donelick,R.A.,Balestrieri,M.L.,et al.,2009.Reproducibility of Apatite Fission-Track Length Data and Thermal History Reconstruction.Earth and Planetary Science Letters,284(3-4):504-515.https://doi.org/10.1016/j.tifl.2009.05.015
Ketcham,R.A.,Donelick,R.A.,Carlson,W.D.,1999.Variability of Apatite Fission-Track Annealing Kinetics;III,Extrapolation to Geological Time Scales.American Mineralogist,84(9):1235-1255.https://doi.org/10.2138/am-1999-0903
Laslett,G.M.,Green,P.F.,Duddy,I.R.,et al.,1987.Thermal Annealing of Fission Tracks in Apatite 2.A Quantitative Analysis.Chemical Geology:Isotope Geoscience Section,65(1):1-13.https://doi.org/10.1016/0168-9622(87)90057-1
Li,R.Y.,Mei,L.F.,Zhu,G.H.,et al.,2013.Late Mesozoic to Cenozoic Tectonic Events in Volcanic Arc,West Burma Block:Evidences from U-Pb Zircon Dating and Apatite Fission Track Data of Granitoids.Journal of Earth Science,24(4):553-568.https://doi.org/10.1007/s12583-013-0349-7
Licht,A.,France-Lanord,C.,Reisberg,L.,et al.,2013.APalaeo Tibet-Myanmar Connection?Reconstructing the Late Eocene Drainage System of Central Myanmar Using a Multi-Proxy Approach.Journal of the Geological Society,170(6):929-939.https://doi.org/10.1144/jgs2012-126
Licht,A.,Reisberg,L.,France-Lanord,C.,et al.,2015.Cenozoic Evolution of the Central Myanmar Drainage System:Insights from Sediment Provenance in the Minbu Sub-Basin.Basin Research,28(2):237-251.https://doi.org/10.13039/501100003135
Maurin,T.,Rangin,C.,2009.Structure and Kinematics of the Indo-Burmese Wedge:Recent and Fast Growth of the Outer Wedge.Tectonics,28(2):TC2010.https://doi.org/10.1029/2008tc002276
Metcalfe,I.,2011.Tectonic Framework and Phanerozoic Evolution of Sundaland.Gondwana Research,19(1):3-21.https://doi.org/10.1016/j.gr.2010.02.016
Metcalfe,I.,2013.Gondwana Dispersion and Asian Accretion:Tectonic and Palaeogeographic Evolution of Eastern Tethys.Journal of Asian Earth Sciences,66:1-33.https://doi.org/10.1016/j.jseaes.2012.12.020
Mitchell,A.,Chung,S.L.,Oo,T.,et al.,2012.Zircon U-Pb Ages in Myanmar:Magmatic-Metamorphic Events and the Closure of a Neo-Tethys Ocean?Journal of Asian Earth Sciences,56:1-23.https://doi.org/10.1016/j.jseaes.2012.04.019
Mitchell,A.H.G.,1993.Cretaceous-Cenozoic Tectonic Events in the Western Myanmar(Burma)-Assam Region.Journal of the Geological Society,150(6):1089-1102.https://doi.org/10.1144/gsjgs.150.6.1089
Naing,T.T.,Bussien,D.A.,Winkler,W.H.,et al.,2013.Provenance Study on Eocene-Miocene Sandstones of the Rakhine Coastal Belt,Indo-Burman Ranges of Myanmar:Geodynamic Implications.Geological Society,London,Special Publications,386(1):195-216.https://doi.org/10.1144/SP386.10
Nielsen,C.,Chamot-Rooke,N.,Rangin,C.,2004.From Partial to Full Strain Partitioning along the Indo-Burmese Hyper-Oblique Subduction.Marine Geology,209(1-4):303-327.https://doi.org/10.1016/j.margeo.2004.05.001
Oo,K.L.,Zaw,K.,Meffre,S.,et al.,2015.Provenance of the Eocene Sandstones in the Southern Chindwin Basin,Myanmar:Implications for the Unroofing History of the Cretaceous-Eocene Magmatic Arc.Journal of Asian Earth Sciences,107:172-194.https://doi.org/10.1016/j.jseaes.2015.04.029
Pal,T.,Chakraborty,P.P.,Gupta,T.D.,et al.,2003.Geodynamic Evolution of the Outer-Arc-Forearc Belt in the Andaman Islands,the Central Part of the Burma-Java Subduction Complex.Geological Magazine,140(3):289-307.https://doi.org/10.1017/S0016756803007805
Pivnik,D.A.,Nahm,J.,Tucker,S.,et al.,1998.Polyphase Deformation in a Fore-Arc/Back-Arc Basin,Salin Subbasin,Myanmar(Burma).American Association of Petroleum Geologists Bulletin,82:1837-1856.https://doi.org/10.1306/1d9bd15f-172d-11d7-8645000102c1865d
Searle,M.P.,Noble,S.R.,Cottle,J.M.,et al.,2007.Tectonic Evolution of the Mogok Metamorphic Belt,Burma(Myanmar)Constrained by U-Th-Pb Dating of Metamorphic and Magmatic Rocks.Tectonics,26(3):TC3014.https://doi.org/10.1029/2006tc002083
Shen,C.B.,Mei,L.F.,Liu,Z.Q.,et al.,2009.Apatite and Zircon Fission Track Data,Evidences for the MesozoicCenozoic Uplift of Huangling Dome,Central China.Journal of Mineralogy and Petrology,29(2):45-60(in Chinese with English abstract).
Wandrey,C.J.,2006.Eocene to Miocene Composite Total Petroleum System,Irrawaddy-Andaman and North Burma Geologic Provinces,Myanmar,Chapter E.In:Wandrey,C.J.,ed.,Petroleum Systems and Related Geologic Studies in Region 8,South Asia.Geological Survey Bulletin,2208:26.
Wang,J.G.,Wu,F.Y.,Tan,X.C.,et al.,2014.Magmatic Evolution of the Western Myanmar Arc Documented by U-Pb and Hf Isotopes in Detrital Zircon.Tectonophysics,612-613:97-105.https://doi.org/10.1016/j.tecto.2013.11.03
Xie,N.,Jiang,Y.,Zhu,G.H.,et al.,2010.Evolution of the Sagaing Strike-Slip Fault and Its Control of Shuibo Basin Structural Evolution,Myanmar.Geoscience,24(2):268-272(in Chinese with English abstract).
Zhang,P.,Mei,L.F.,Ma,Y.X.,et al.,2014.Tectonic Features and Dynamic Evolution of Bay of Bengal Basin:New Insights into Satellite-Gravity and Seismic Data.Earth Science,39(10):1307-1321(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2014.123
Zhang,P.,Mei,L.F.,Hu,X.L.,et al.,2017a.Structures,Uplift,and Magmatism of the Western Myanmar Arc:Constraints to Mid-Cretaceous-Paleogene Tectonic Evolution of the Western Myanmar Continental Margin.Gondwana Research,52:18-38.https://doi.org/10.1016/j.gr.2017.09.002
Zhang,P.,Mei,L.F.,Xiong,P.,et al.,2017b.Structural Features and Proto-Type Basin Reconstructions of the Bay of Bengal Basin:A Remnant Ocean Basin Model.Journal of Earth Science,28(4):666-682.https://doi.org/10.1007/s12583-017-0750-8
陈贺贺,朱筱敏,黄捍东,等,2017.基于碎屑锆石定年的饶阳凹陷蠡县斜坡沙河街组物源分析.地球科学,42(11):1955-1971.https://doi.org/10.3799/dqkx.2017.124
沈传波,梅廉夫,刘昭茜,等,2009.黄陵隆起中-新生代隆升作用的裂变径迹证据.矿物岩石,29(2):45-60.
谢楠,姜烨,朱光辉,等,2010.缅甸Sagaing走滑断裂及对睡宝盆地构造演化的控制和影响.现代地质,24(2):268-272.
张朋,梅廉夫,马一行,等,2014.孟加拉湾盆地构造特征与动力学演化:来自卫星重力与地震资料的新认识.地球科学,39(10):1307-1321.https://doi.org/10.3799/dqkx.2014.123