WANG Yu1, HE Dengfa2, LIU Songnan1, ZHOU Liyun1, GAO Shanlin3
1 Institute of Earth Sciences,China University of Geosciences(Beijing),Beijing 100083,China; 2 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083,China; 3 Petroleum Exploration and Production Branch of SINOPEC,Beijing 100728,China;
Abstract：The palaeogeography is to study and understand the earth-surface environment in the geological histories,and it is a product of tectonics-environment(climate)-sedimentation interaction and reaction. The traditional palaeogeography and related tectono-palaeogeography,biopalaeogeography and other subjects have given great contributions to the tectonic evolution,continental reconstruction as well oil-gas exploration and development. More and more works start to focus on the interaction of multiple-layers of the earth,especially the paleo-climate,paleo-environment studies,it's necessary to integrate the earth-surface environment and the tectonic background to reveal the influence of the deep and shallow layers geologic processes on the palaeogeographic framework formation and evolution. We propose a new concept and subject—chrono-palaeogeography to explore the earth surface process and evolution in the geological history. This subject is in a precise isotopic chronological framework to study how the different dynamics-kinematic-material transferring-environment changes shaped the palaeogeography,or how the palaeogeographic framework responded to the interactions or couplings of the materials-tectonics stress-environment(climate). Better than other subjects of the palaeogeography,this subject is for studying and understanding the earth-surface process,but not the environmental state,or the active process to form the earth-surface environment. We emphasize the multiple kinetic factors in a same time,the variation in different spaces,and the diachronous at various scales. In addition,we introduce a few case studies of high precise time constrained palaeogeographic work,such as those studies on the Chinese Taiwan,Yangtze and North China cratons,to show how chrono-palaeogeography improve reconstruction of the continent,tectonic evolution,as well oil-gas exploration.
[1] 陈洪德,侯明才,陈安清,时志强,邢凤存,黄可可,刘欣春. 2017. 中国古地理学研究进展与关键科学问题. 沉积学报, 35(5): 888-901. [Chen H D,Hou M C,Chen A Q,Shi Z Q,Xing F C,Huang K K,Liu X C.2017. Advances and the major scientific issues of the paleogeography in China. Acta Sedimentologica Sinica, 35(5): 888-901] [2] 《地球科学大辞典》编委会. 2006. 地球科学大辞典(基础学科卷). 北京: 地质出版社, 777. [Editorial board of the Great Dictionary of Earth Sciences. 2006. The Great Dictionary of Earth Sciences(Basic Science Volume). Beijing: Geological Publishing House,777] [3] 冯增昭. 2003. 我国古地理学的形成、发展、问题和共识. 古地理学报, 5(2): 129-141. [Feng Z Z.2003. Origin,development,problems and common viewpoint of palaeogeography of China. Journal of Palaeogeography(Chinese Edition), 5(2): 129-141] [4] 冯增昭. 2009. 中国古地理学的定义、内容、特点和亮点. 古地理学报, 11(1): 1-11. [Feng Z Z.2009. Definition,content,characteristics and bright spots of palaeogeography of China. Journal of Palaeogeography(Chinese Edition), 11(1): 1-11] [5] 蒋维红,董春梅,闫家宁. 2007. 岩相古地理学研究现状及发展趋势. 断块油气田, 14(3): 1-4. [Jiang W H,Dong C M,Yan J N.2007. Study on present situation and trend of lithofacies paleogeography. Fault-block Oil & Gasfield, 14(3): 1-4] [6] 莱伊尔. 1830. 地质学原理(中文版). 北京: 北京大学出版社,1-660. [Lyell C.1830. Principles of Geology(Chinese Edition). Beijing: Peking University Press, 1-660] [7] 刘少峰,王成善. 2016. 构造古地理重建与动力地形. 地学前缘, 23(6): 61-79. [Liu S F,Wang C S.2016. Reconstruction of tectono-paleogeography and dynamic topography. Earth Science Frontiers, 23(6): 61-79] [8] 马宗晋,高祥林,杜品仁. 2006. 全球表层系统研究的思考. 地学前缘, 13(6): 96-101. [Ma Z J,Gao X L,Du P R.2006. Pondering over the study on the outermost sphere system of the Earth. Earth Science Frontiers, 13(6): 96-101] [9] 王训练,吴怀春. 2016. 地球系统科学时代的高分辩综合地层学. 地学前缘, 23(6): 246-252. [Wang X L,Wu H C.2016. High resolution integrated stratigraphy in the age of Earth system science. Earth Science Frontiers, 23(6): 246-252] [10] 张元元,曾宇轲,唐文斌. 2021. 准噶尔盆地西北缘二叠纪原型盆地分析. 石油科学通报, 6(3): 333-343. [Zhang Y Y,Zeng Y K,Tang W B.2021. Permian attributes and tectonic evolution of the west Junggar Basin. Petroleum Science Bulletin, 6(3): 333-343] [11] 郑秀娟,鲍志东,冯增昭. 2013.21世纪初十年中国古地理学发展概要. 矿物岩石地球化学通报, 35(3): 301-309. [Zheng X J,Bao Z D,Feng Z Z.2013. Advance of palaeogeography in China in the first 10 years of the 21st Century. Bulletin of Mineralogy, Petrology and Geochemistry, 32(3): 301-309] [12] Bird P.2003. An updated digital model of plate boundaries. Geochemistry,Geophysics, Geosystems, 4: 1027-1052. [13] Conrad C,Lithgow-Bertelloni C.2002. How mantle slabs drive plate tectonics. Science, 298: 207-209. [14] Doglioni C,Carminati E,Cuffaro M,Scrocca D.2007. Subduction kinematics and dynamic constraints. Earth-Science Reviews, 83: 125-175. [15] Flament N.2014. Linking plate tectonics and mantle flow to Earth's topography. Geology, 42: 927-928. [16] Flament N,Gurnis M,Williams S,Seton M,Skogseid J,Heine C,Müller R D.2014. Topographic asymmetry of the South Atlantic from global models of mantle flow and lithospheric stretching. Earth and Planetary Science Letter, 387: 107-119. [17] Gao L,Liu S W,Cawood P A,Hu F Y,Wang J T,Sun G Z,Hu Y L.2022. Oxidation of Archean upper mantle caused by crustal recycling. Nature Communications, 13: 3283. [18] Gerya T.2011. Future directions in subduction modelling. Journal of Geodynamics, 52: 344-378. [19] Govers R,Wortel R.2005. Lithosphere tearing at STEP faults: response to edges of subduction zones. Earth and Planetary Science Letters, 236: 505-523. [20] Gurnis M,Turner M,Zahirovic S,DiCaprio L,Spasojevic S,Müller R D,Boyden J,Seton M,Manea V C,Bower D J.2012. Plate tectonic reconstructions with continuously closing plates. Computers and Geosciences, 38: 35-42. [21] Hall R.2012. Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian Ocean. Tectonophysics, 570-571: 1-41. [22] Hu S B,Raza A,Min K,Kohn B P,Reiners P W,Ketcham R A,Wang J Y,Gleadow A J W.2006. Late Mesozoic and Cenozoic thermotectonic evolution along a transect from the north China craton through the Qinling orogen into the Yangtze craton,central China. Tectonics, 25: TC6009. doi: 10.1029/2006TC001985. [23] Johnson M R W, Harley S L. 2015. Orogenesis:the Making of Mountains. Cambridge University Press, 1-374. [24] Liu J H,Zhang P Z,Lease R O,Zheng D W,Wan J L,Wang W T,Zhang H P.2013. Eocene onset and late Miocene acceleration of Cenozoic intracontinental extension in the North Qinling range-Weihe graben: insights from apatite fission track thermochronology. Tectonophysics, 584: 281-296. [25] Mao Q G,Xiao W J,Windley B F,Han C M,Qu J F,Ao S J,Zhang J E,Guo Q Q.2012. The Liuyuan complex in the Beishan,NW China: a Carboniferous-Permian ophiolitic fore-arc sliver in the southern Altaids. Geological Magazine, 149: 483-506. [26] McDougall I,Harrison T M. 1999. Geochronology and thermochronology by the 40Ar/39Ar method. New York and Oxford University Press, 1-269. [27] Mineralogical Society of America. 2017. Petrochronology: methods and applications. Reviews in Mineralogy and Geochemistry, 83(1): 1-575. [28] Mueller S,Phillips R.1991. On the initiation of subduction. Journal of Geophysical Research, 96: 651-665. [29] Müller R D,Seton M,Zahirovic S,Williams E S,Matthews J K,Wright M N,Shephard E G,Maloney T K,Barnett-Moore N,Hosseinpour M,Bower J D,Cannon J.2016. Ocean basin evolution and global-scale plate reorganization events since Pangea breakup. Annual Review of Earth and Planetary Sciences, 44: 107-138. [30] Reiners P W,Carlson R W,Renne P R,Cooper K M,Granger D E,McLean N M,Schoene B.2018. Geochronology and thermochronology. American Geophysical Union, John Wiley and Sons, 1-464. [31] Unsworth M.2009. A plate boundary in flux. Nature Geoscience, 2: 605-606. [32] van der Haeghe O.2012. The thermal mechanical evolution of crustal orogenic belts at convergent plate boundaries: a reappraisal of the orogenic cycle. Journal of Geodynamics, 56-57: 124-145. [33] Wang Y,Zhou L Y,Zhao L J,Ji M,Gao H L.2010. Palaeozoic uplands and unconformity in the North China Block: constraints from zircon LA-ICP-MS dating and geochemical analysis of Bauxite. Terra Nova, 22: 264-273. [34] Wang Y,Luo Z H,Wu P,Cheng L L,Hao J H.2014. A new interpretation of the sedimentary environment before and during eruption of the Emeishan LIP,Southwest China. International Geology Review, 56: 1295-1313. [35] Wang Y,Luo Z H,Santosh M,Wang S Z,Wang N.2017. The Liuyuan Volcanic Belt in NW China revisited: evidence for Permian rifting associated with the assembly of continental blocks in the Central Asian Orogenic Belt. Geological Magazine, 154: 265-285. [36] Wang Y,Sun L X,Zhou L Y,Xie Y T.2018. Discussion on the relationship between the Yanshanian Movement and cratonic destruction in North China. Science in China(Earth Sciences), 61: 499-514. [37] Wang Y,Ukstins Peate I,Luo Z H,Wang S Z,Cheng L L,Hao J H,Wang Y.2019. Rifting in SW China: structural and sedimentary investigation of the initial crustal response to emplacement of the Permian Emeishan LIP. Geological Magazine, 156: 745-758. [38] Wang Y,Zhou L Y,Zwingmann H,Lo C-H,Li G W,Hao J H.2020.40Ar/39Ar dating of cataclastic K-feldspar: a new approach for establishing the chronology of brittle deformation. Journal of Structural Geology, 131: 103948. [39] Liu S N,Wang Y.2022. Origin of the Songpan-Garze Terrane on the northeastern Tibetan Plateau,eastern segment of the Tethyan tectonic domain: a Middle Permian-Early Triassic intracontinental rifting system. Geological Society of America Bulletin,in press. [40] Yui T F,Maki K,Lan C Y,Hirata T,Chu H T,Kon Y,Yokoyama T D,Jahn B M,Ernst W G.2012. Detrital zircons from the Tananao metamorphic complex of Taiwan: implications for sediment provenance and Mesozoic tectonics. Tectonophysics, 541-543: 31-42. [41] Zhang Y Y,Dostal J,Zhao Z H,Liu C,Guo Z J.2011. Geochronology,geochemistry and petrogenesis of mafic and ultramafic rocks from Southern Beishan area,NW China: implications for crust-mantle interaction. Gondwana Research, 20: 816-830.
