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Volume 40 Issue 1
Jan.  2021
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Article Navigation >  Bulletin of Geological Science and Technology  > 2021  >  40(1): 27-35, 48
Wang Ying, Xin Renchen. Evolution and geodynamic background of Myanmar petroliferous basin group[J]. Bulletin of Geological Science and Technology, 2021, 40(1): 27-35, 48. doi: 10.19509/j.cnki.dzkq.2021.0009
Citation: Wang Ying, Xin Renchen. Evolution and geodynamic background of Myanmar petroliferous basin group[J]. Bulletin of Geological Science and Technology, 2021, 40(1): 27-35, 48. doi: 10.19509/j.cnki.dzkq.2021.0009
shu

Evolution and geodynamic background of Myanmar petroliferous basin group

doi: 10.19509/j.cnki.dzkq.2021.0009
  • Received Date: 08 Jan 2020
    Abstract
  • Based on the analysis of the geological records of different tectonic units, and combined with plate reconstruction and geodynamic background, the evolution and their geodynamic background of Myanmar petroliferous basin group are discussed in this paper.The study shows that the basement of Myanmar petroliferous basin group is a metamorphic complex developed in the Late Cimmerian period.From Late Cretaceous to Eocene, the Neo-Tethys oceanic crust subducted towards the NNE under the West Burma block.Accretionary wedge developed on the western edge of the West Burma block, and volcanic arcs, fore-arc rift basins, and back-arc rift basins formed in the West Burma block.Since Oligocene, the Neo-Tethys closed down, and then the Indian block and the northern part of the West Burma block collided, and the basins in the northern part of the West Burma block evolved into back-arc foreland basins.The Indian Ocean crust subducted towards the NEE under the central and southern parts of West Burma block, and the accretionary wedge developed on the western edge of the West Burma block gradually uplifted to the Indo-Burma range.The central and southern basins of the West Burma block on the east side of the Indo-Burma range all evolved into back-arc compressional basins, while the Rakhine basin on the west side of the Indo-Burma range evolved into fore-arc basin.The results of this study have certain indicative significance for the prediction and exploration of oil-gas and mineral resources in the Myanmar basin group.

     

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    • References(46)
  • [1]
    王宏, 林方成, 李兴振, 等.缅甸中北部及邻区构造单元划分及新特提斯构造演化[J].中国地质, 2012, 39(4):912-922. doi: 10.3969/j.issn.1000-3657.2012.04.006
    [2]
    张舜尧, 马立祥, 梅廉夫, 等.缅甸及其周缘区域新生代沉积物源分析及沉积体系分布[J].地质科技情报, 2011, 30(5):29-35. doi: 10.3969/j.issn.1000-7849.2011.05.006
    [3]
    Li J X, Zhang L Y, Fan W M, et al.Mesozoic-Cenozoic tectonic evolution and metallogeny in Myanmar:Evidence from zircon/cassiterite U-Pb and molybdenite Re-Os geochronology[J].Ore Geology Reviews, 2018, 102:829-845. doi: 10.1016/j.oregeorev.2018.10.009
    [4]
    陈希节, 许志琴, Sein K, 等.缅甸中部抹谷早白垩世构造岩浆作用及对特提斯演化的启示[J].地质学报, 2016, 90(11):3060-3080. doi: 10.3969/j.issn.0001-5717.2016.11.007
    [5]
    Mitchell A, Chung S L, Oo T, et al.Zircon U-Pb ages in Myanmar:Magmatic-metamorphic events and the closure of a neo-Tethys ocean?[J].Journal of Asian Earth Sciences, 2012, 56:1-23. doi: 10.1016/j.jseaes.2012.04.019
    [6]
    Morley C K, Naing T T, Searle M, et al.Structural and tectonic development of the Indo-Burma Ranges[J].Earth-Science Reviews, 2019, 200:1-43.
    [7]
    Wang J G, Wu F Y, Tan X C, et al.Magmatic evolution of the Western Myanmar Arc documented by U-Pb and Hf isotopes in detrital zircon[J].Tectonophysics, 2014, 612/613:97-105. doi: 10.1016/j.tecto.2013.11.039
    [8]
    Li R Y, Mei L F, Zhu G H, et al.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[J].Journal of Earth Science, 2013, 24(4):553-568. doi: 10.1007/s12583-013-0349-7
    [9]
    Oo K L, Zaw K, Meffre S, et al.Provenance of the Eocene sandstones in the southern Chindwin Basin, Myanmar:Implications for the unroofing history of the Cretaceous-Eocene magmatic arc[J].Journal of Asian Earth Sciences, 2015, 107:172-194. doi: 10.1016/j.jseaes.2015.04.029
    [10]
    赖生华, 麻建明, 廖林.缅甸中央沉降带Chindwin盆地油气勘探潜力[J].天然气工业, 2005, 25(11):21-24. doi: 10.3321/j.issn:1000-0976.2005.11.007
    [11]
    谢楠, 赵汝敏.缅甸Shwebo盆地油气地质特征及勘探潜力[J].天然气地球科学, 2014, 25(4):558-564. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201404011.htm
    [12]
    李任远, 梅廉夫, 胡孝林, 等.缅甸中央盆地北部新生代古地貌重建[J].地质科技情报, 2018, 37(3):126-133. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201803017.htm
    [13]
    Win M M, Enami M, Kato T.Metamorphic conditions and CHIME monazite ages of Late Eocene to Late Oligocene high-temperature Mogok metamorphic rocks in central Myanmar[J].Journal of Asian Earth Sciences, 2016, 117:304-316. doi: 10.1016/j.jseaes.2015.11.023
    [14]
    张舜尧, 马立祥, 杨志斌, 等.主动大陆边缘增生楔构造发育及沉积特征分析:以缅甸增生楔为例[J].地质科技情报, 2015, 34(1):89-94. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201501014.htm
    [15]
    Zhang J E, Xiao W J, Windley B F, et al.Early Cretaceous wedge extrusion in the Indo-Burma Range accretionary complex:implications for the Mesozoic subduction of Neotethys in SE Asia[J].International Journal of Earth Sciences, 2017, 106(4):1391-1408. doi: 10.1007/s00531-017-1468-7
    [16]
    Dey A, Hussain M F, Barman M N.Geochemical characteristics of mafic and ultramafic rocks from the Naga Hills Ophiolite, India:Implications for petrogenesis[J].Geoscience Frontiers, 2018, 9(2):517-529. doi: 10.1016/j.gsf.2017.05.006
    [17]
    Acharyya S K.Indo-Burma Range:A belt of accreted microcontinents, ophiolites and Mesozoic-Paleogene flyschoid sediments[J].International Journal of Earth Sciences, 2015, 104(5):1235-1251. doi: 10.1007/s00531-015-1154-6
    [18]
    Acharyya S K.Collisional emplacement history of the Naga-Andaman ophiolites and the position of the eastern Indian suture[J].Journal of Asian Earth Sciences, 2007, 29(2):229-242.
    [19]
    IHS.Rakhine Basin[EB/OL].(2008-08) https://edin.ihsenergy.com/edingis/servlet/SSOLogin.
    [20]
    王雪峰, 吕福亮, 范国章, 等.孟加拉湾若开盆地构造特征及演化[J].成都理工大学学报:自然科学版, 2013, 40(4):424-430. doi: 10.3969/j.issn.1671-9727.2013.04.10
    [21]
    Moore G F, Aung L T, Fukuchi R, et al.Tectonic, diapiric and sedimentary chaotic rocks of the Rakhine coast, western Myanmar[J].Gondwana Research, 2019, 74:126-143. doi: 10.1016/j.gr.2019.04.006
    [22]
    邱春光, 朱光辉, 谢晓军, 等.主动大陆边缘海沟-斜坡盆地沉积体系分析:以缅甸若开海岸盆地某工区为例[J].沉积与特提斯地质, 2011, 31(3):13-19. doi: 10.3969/j.issn.1009-3850.2011.03.003
    [23]
    唐鹏程, 邵大力, 王海强, 等.孟加拉湾若开海域晚新生代构造变形及其对油气的控制作用[J].海相油气地质, 2016, 21(1):52-60. doi: 10.3969/j.issn.1672-9854.2016.01.008
    [24]
    Ridd M F.East flank of the Sibumasu block in NW Thailand and Myanmar and its possible northward continuation into Yunnan:A review and suggested tectono-stratigraphic interpretation[J].Journal of Asian Earth Sciences, 2015, 104:160-174. doi: 10.1016/j.jseaes.2014.01.023
    [25]
    Metcalfe I, Aung K P.Late Tournaisian conodonts from the Taungnyo Group near Loi Kaw, Myanmar(Burma):Implications for Shan Plateau stratigraphy and evolution of the Gondwana-derived Sibumasu Terrane[J].Gondwana Research, 2014, 26(3/4):1159-1172. http://www.sciencedirect.com/science/article/pii/S1342937X13002992
    [26]
    Cai F L, Lin D, Wei Y, et al.Provenance and tectonic evolution of Lower Paleozoic-Upper Mesozoic strata from Sibumasu terrane, Myanmar[J].Gondwana Research, 2017, 41:325-336. doi: 10.1016/j.gr.2015.03.005
    [27]
    Jiang H, Li W Q, Jiang S Y, et al.Geochronological, geochemical and Sr-Nd-Hf isotopic constraints on the petrogenesis of Late Cretaceous A-type granites from the Sibumasu Block, Southern Myanmar, SE Asia[J].Lithos, 2017, 268/271:32-47. doi: 10.1016/j.lithos.2016.11.005
    [28]
    Yao W, Ding L, Cai F, et al.Origin and tectonic evolution of upper Triassic turbidites in the Indo Burman ranges, West Myanmar[J].Tectonophysics, 2017, 721:90-105. doi: 10.1016/j.tecto.2017.09.016
    [29]
    IHS.Chindwin Basin[EB/OL].(2008-08) https://edin.ihsenergy.com/edingis/servlet/SSOLogin.
    [30]
    Zhang P, Mei L, Hu X L, et al.Structures, uplift, and magmatism of the Western Myanmar Arc:Constraints to mid-Cretaceous-Paleogene tectonic evolution of the western Myanmar continental margin[J].Gondwana Research, 2017, 52:18-38. doi: 10.1016/j.gr.2017.09.002
    [31]
    李运振, 赵汝敏, 赵厚祥.火山岛弧带对盆地沉积体系形成与分布的影响:以缅甸陆上钦敦-睡宝盆地某区块为例[J].地质科技情报, 2014, 33(3):36-43. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201403005.htm
    [32]
    Myitta K K.Marine transgression and regression in Miocene sequences of northern Pegu(Bago) Yoma, Central Myanmar[J].Journal of Asian Earth Sciences, 1999, 17(3):369-393. doi: 10.1016/S0743-9547(98)00065-8
    [33]
    Licht A, Dupont-Nivet G, Win Z, et al.Paleogene evolution of the Burmese forearc basin and implications for the history of India-Asia convergence[J].Geological Society of America Bulletin, 2019, 131(5/6):730-748. http://www.onacademic.com/detail/journal_1000042302890899_e004.html
    [34]
    王二七, 孟恺, 许光, 等.印度陆块新生代两次仰冲事件及其构造驱动机制:论印度洋、特提斯和欧亚板块相互作用[J].岩石学报, 2018, 34(7):1867-1875. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201807003.htm
    [35]
    Metcalfe I.Gondwana dispersion and Asian accretion:Tectonic and palaeogeographic evolution of eastern Tethys[J].Journal of Asian Earth Sciences, 2013, 66:1-33. doi: 10.1016/j.jseaes.2012.12.020
    [36]
    史毅, 屈红军, 宫臣兴, 等.东特提斯的形成演化及其典型蛇绿岩带地质特征[J].地质科技情报, 2018, 37(6):31-36. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201806004.htm
    [37]
    王茜, 辛仁臣, 董瑞杰, 等.喜马拉雅前渊和孟加拉湾盆地形成演化[J].海洋地质前沿, 2018, 34(11):10-19. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT201811002.htm
    [38]
    覃琼, 徐亚东, 郑国栋, 等.滇西剑川盆地剑川组岩石特征及火山喷发-沉积期次[J].地质科技情报, 2019, 38(5):165-173. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201905017.htm
    [39]
    Van Hinsbergen D J J, Steinberger B, Doubrovine P V, et al.Acceleration and deceleration of India-Asia convergence since the Cretaceous:Roles of mantle plumes and continental collision[J].Journal of Geophysical Research:Solid Earth, 2011, 116(B6):1-20. doi: 10.1029/2010JB008051/full
    [40]
    Lee T Y, Lawver L A.Cenozoic plate reconstruction of Southeast Asia[J].Tectonophysic, 1995, 251(1/4):85-138. http://www.sciencedirect.com/science/article/pii/0040195195000232
    [41]
    张海坤, 胡鹏, 曹亮, 等.印度尼西亚戴里Sedex型铅锌矿集区成矿流体特征及成矿物质来源:流体包裹体及同位素地球化学证据[J].地质科技通报, 2020, 39(3):170-177. http://dzkjqb.cug.edu.cn/CN/abstract/abstract10034.shtml
    [42]
    Metcalfe I.ASIA|South-East, in encyclopedia of geology[M].Oxford:Elsevier.2005.
    [43]
    Metcalfe I.Palaeozoic-Mesozoic history of SE Asia[J].Geological Society, 2011, 355(1):7-35. doi: 10.1144/SP355.2
    [44]
    Hall R.Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian Ocean[J].Tectonophysics, 2012, 570-571:1-41. doi: 10.1016/j.tecto.2012.04.021
    [45]
    Curray J R.The Bengal depositional system:From rift to orogeny[J].Marine Geology, 2014, 352:59-69. doi: 10.1016/j.margeo.2014.02.001
    [46]
    Khin K, Sakai T, Zaw K.Neogene syn-tectonic sedimentation in the eastern margin of Arakan-Bengal basins, and its implications on for the Indian-Asian collision in western Myanmar[J].Gondwana Research, 2014, 26(1):89-111. doi: 10.1016/j.gr.2013.04.012
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