Concept,model,formation and disordered variation of Ocean Plate Stratigraphy
Xu Shu-Mei1,2,3, Kong Jia-Hao1,2, Li San-Zhong1,2,3, Shu Peng-Cheng1,2, Ma Hui-Lei1,2, Cui Hui-Qi1,2
1 Key Lab of Submarine Geosciences and Prospecting Techniques,Ministry of Education, Ocean University of China, Shandong Qingdao 266100,China; 2 College of Marine Geosciences,Ocean University of China,Shandong Qingdao 266100,China; 3 Institute of Advanced Oceanography/Frontiers Science Center for Deep Ocean Multispheres and Earth System,Shandong Qingdao 266100,China
Abstract This paper mainly focuses on the concept,model,formation and disordered variation of the Ocean Plate Stratigraphy(OPS). The sedimentary records of the ancient ocean floor after subduction and collision include the orogenic mélange and continental margin accretionary complexes,which can be reconstructed by micropaleontology and isotope chronology. The reconstructed stratigraphy from the mélange and accretion complex is here referred to as “Ocean Plate Stratigraphy”. The basic composition of OPS reconstructed from the mélange and accretive complexes of orogenic belts is similar,but the composition and types of OPS are different due to the different magma background of oceanic lithosphere. The paper introduces how to re-establish OPS from the accretive orogenic belt undergoing subduction and collision based on different types of oceanic plate strata. The purpose of introducing the concept of OPS is to re-establish the stratigraphic units of the vanished ocean basin and marginal sea basin. It will play a positive role in promoting the stratigraphic analysis of orogenic belt,in restoring the orogenic belt tectonic paleogeography,and in studying the paleogeography during major tectonic changes and plate reconstruction.
Fund:Co-funded by the National Natural Science Foundation of China(Nos. 91958109,91958214, 42121005),the Basic Research Project for the Central Universities(No.202172003),the Joint Project of the National Natural Science Foundation of China and Shandong Marine Science Center(No. U1606401),and the Taishan Scholars�� Climbing Program of Shandong Province(No. tspd20210315)
About author: Xu Shumei,born in 1970, professor, is engaged in studies on sedimentology and basin analysis.E-mail: xsm@ouc.edu.cn.
Cite this article:
Xu Shu-Mei,Kong Jia-Hao,Li San-Zhong et al. Concept,model,formation and disordered variation of Ocean Plate Stratigraphy[J]. JOPC, 2022, 24(1): 1-10.
Xu Shu-Mei,Kong Jia-Hao,Li San-Zhong et al. Concept,model,formation and disordered variation of Ocean Plate Stratigraphy[J]. JOPC, 2022, 24(1): 1-10.
[1]蔡雄飞,刘德民. 2005. 造山带古海洋恢复的思路和研究方法. 海洋地质动态, 21(7): 33-36. [Cai X F,Liu D M.2005. Reversed order: a new method for restoration of an ancient ocean in orogenic belt. Marine Geology Letters, 21(7): 33-36] [2]蔡雄飞. 2006. 试论造山带层序地层的类型、特点和控制因素: 以东昆仑三叠系为例. 地层学杂志, 30(2): 131-135. [Cai X F.2006. The orogenic sequence stratigraphic types and their controlling factor taking the Triassic of eastern Kunlun as example. Journal of Stratigraphy, 30(2): 131-135] [3]杜远生,颜佳新,韩欣. 1995. 造山带沉积地质学研究的新进展. 地质科技情报, 14(1): 29-34. [Du Y S,Yan J X,Han X.1995. New progress in sedimentary geology of orogenic belt. Geological Science and Technology Information, 14(1): 29-34] [4]杜远生,盛吉虎,丁振举. 1997. 造山带非史密斯地层及其地质制图. 中国区域地质, 16(4): 439-443. [Du Y S,Sheng J H,Ding Z J.1997. Non-Smith Strata in the orogen and their geological mapping. Regional Geology of China, 16(4): 439-443] [5]杜远生,张克信. 1999. 关于非史密斯地层学的几点认识. 地层学杂志, 23(1): 78-80. [Du Y S,Zhang K X.1999. Discussions on Non-Smith Stratigraphy. Journal of Stratigraphy, 23(1): 78-80] [6]冯庆来,叶玫. 2000. 造山带区域地层学研究的理论、方法和实例剖析. 武汉: 中国地质大学出版社,1-94. [Feng Q L,Ye M.2000. Theory,method and case study of regional stratigraphy in orogenic belt. Wuhan: China University of Geosciences Press,1-94] [7]吴根耀. 2003. 初论造山带古地理学. 地层学杂志, 27(2): 81-98. [Wu G Y.2003. An approach to orogen paleogeography. Journal of Stratigraphy, 27(2): 81-98] [8]吴浩若. 1992. 构造地层学. 地球科学进展, 7(2): 75. [Wu H R.1992. Tectostratigraphy. Advance in Earth Science, 7(2): 75] [9]杨经绥,徐向珍,李天福,陈松永,任玉峰,李金阳,刘钊. 2011. 新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年: 早古生代洋盆的证据. 岩石学报, 27(1): 77-95. [Yang J S,Xu X Z,Li T F,Chen S Y,Ren Y F,Li J Y,Liu Z.2011. U-Pb ages of zircons from ophiolite and related rocks in the Kumishi region at the southern margin of Middle Tianshan,Xinjiang: evidence of Early Paleozoic oceanic basin. Acta Petrologica Sinica, 27(1): 77-95] [10]张克信,殷鸿福,朱云海. 2001. 造山带混杂岩区地质填图理论、方法与实践. 武汉: 中国地质大学出版社. [Zhang K X,Yin H F,Zhu Y H. 2001. Theory,Method and Practice of Geological Mapping in Melange Area of Orogenic Belt. Wuhan: China University of Geosciences Press] [11]张克信,殷鸿福,朱云海,王国灿,冯庆来,龚一鸣. 2003. 史密斯地层与非史密斯地层. 地球科学, 28(4): 361-369. [Zhang K X,Yin H F,Zhu Y H,Wang G C, Feng Q L, Gong Y M.2003. Smith strata and non-smith strata. Earth Science, 28(4): 361-369] [12]张克信,冯庆来,宋博文,张智勇,王永和,潘桂棠,陆松年,赵小明,邢光福. 2014. 造山带非史密斯地层. 地学前缘, 21(2): 36-47. [Zhang K X,Feng Q L,Song B W,Zhang Z Y, Wang Y H, Pan G T, Lu S N, Zhao X M, Xing G F.2014. Non-Smithian strata in the orogen. Earth Science Frontiers, 21(2): 36-47] [13]张克信,李仰春,王丽君,王嘉轩,徐亚东,王永和,辛后田. 2020. 造山带混杂岩及相关术语. 地质通报, 39(6): 765-782. [Zhang K X,Li Y C,Wang L J,Wang J X,Xu Y D,Wang Y H,Xin H T.2020. The division of mélanges in the orogenic belt and its associated terminologies. Geological Bulletin of China, 39(6): 765-782] [14]张克信,何卫红,徐亚东,张雄华,宋博文,寇晓虎,王国灿. 2021. 论从俯冲增生杂岩带重建洋板块地层主要类型与序列: 以青藏特提斯二叠系为例. 沉积与特提斯地质, 41(2): 137-151. [Zhang K X,He W H,Xu Y D,Zhang X H,Song B W,Kou X H,Wang G C.2021. Reconstruction of main types for oceanic plate strata in the subduction accretionary complex and feature of sequence for each type: an example from the Qinghai-Tibet Tethyan Permian strata. Sedimentary Geology and Tethyan Geology, 41(2): 137-151] [15]张越,徐学义,陈隽璐,张红英,唐卓,孙小攀,李现冰. 2012. 阿尔泰地区玛因鄂博蛇绿岩的地质特征及其LA-ICP-MS锆石U-Pb年龄. 地质通报, 31(6): 834-842. [Zhang Y,Xu X Y,Chen J L,Zhang H Y,Tang Z,Sun X P,Li X B.2012. Geological characteristics and LA-ICP-MS zircon U-Pb age of Mayinebo ophiolite in Altay orogenic belt. Geological Bulletin of China, 31(6): 834-842] [16]Ando A,Kodama K,Kojima S.2001. Low-latitude and Southern Hemisphere origin of Anisian(Triassic)bedded chert in the Inuyama area,Mino terrane,central Japan. Journal of Geophysical Research, 106: 1973-1986. [17]Cawood P,Kroner A,Collins W,Kusky T M,Mooney W D,Windley B F.2009. Earth accretionary orogens in space and time. Geological Society of London Special Publication, 318: 1-36. [18]Dilek Y,Furnes H.2011. Ophiolite genesis and global tectonics: geochemical and tectonic fingerprinting of ancient oceanic lithosphere. Geological Society of America Bulletin, 123: 387-411. [19]Dobretsov N L,Buslov M M,Safonova I Y,Kokh D A.2004. Fragments of oceanic islands in the Kurai and Katun�� accretionary wedges of Gorny. Russian Geology and Geophysics, 45: 1381-1403. [20]Isozaki Y,Maruyama S,Fukuoka F.1990. Accreted oceanic materials in Japan. Tectonophysics, 181: 179-205. [21]Kimura K,Hori R.1993. Offscraping accretion of Jurassic chert-clastic complexes in the Mino-Tamba Belt,central Japan. Journal of Structural Geology, 15: 145-161. [22]Kusky T M,Wang L,Dilek Y,Robinson P,Peng S B,Huang X Y.2011. Application of the modern ophiolite concept with special reference to Precambrian ophiolites. Science China-Earth Sciences, 54(3): 315-341. [23]Kusky T M,Windley B F,Safonova I,Wakita K,Wakabayashi J,Polat A,Santosh M.2013. Recognition of Ocean Plate Stratigraphy in accretionary orogens through Earth history: a record of 3.8 billion years of seafloor spreading,subduction,and accretion. Gondwana Research, 24: 501-547. [24]Labaume P,Maltman A J,Bolton A,Tessier D,Ogawa Y,Takizawa S.1995. Scaly fabrics in sheared clays from the decollement zone of the Barbados accretionary prism. Proceedings of the Ocean Drilling Program: Scientific Results, 156: 59-77. [25]Mann P,Taira A.2004. Global tectonic significance of the Solomon Islands and Ontong Java Plateau convergent zone. Tectonophysics, 389: 137-190. [26]Maruyama S,Kawai T,Windley B F.2010. Ocean plate stratigraphy and its imbrication in an accretionary orogen: the Mona Complex,Anglesey-Lleyn,Wales,UK. In: Kusky T M,Zhai M G,Xiao W(eds). The Evolving Continents: Understanding Processes of Continental Growth. Geological Society London Special Publications, 338: 55-75. [27]Nakagawa M,Santosh M,Maruyama S.2009. Distribution and mineral assemblages of bedded manganese deposits in Shikoku,Southwest Japan: implications for accretion tectonics. Gondwana Research, 16: 609-621. [28]Pearce J A,Hastie A R,Leat P T,Dalzield I W,Lawverd L A,Barkere P F,Millar I L,Barry T L,Bevins R E.2014. Composition and evolution of the Ancestral South Sandwich Arc: implications for the flow of deep oceanwater and mantle through the Drake Passage Gateway. Global and Planetary Change, 123: 298-322. [29]Regelous M,Hofmann A W,Abouchami W,Galer S J G.2003. Geochemistry of lavas from the Emperor Seamounts,and the geochemical evolution of Hawaiian magmatism from 85 to 42 Ma. Journal of Petrology, 44: 113-140. [30]Safonova I Y,Simonov V A,Buslov M M,Ota T,Maruyama S.2008. Neoproterozoic basalts of the Paleo-Asian Ocean(Kurai accretion zone,Gorny Altai,Russia): geochemistry,petrogenesis,geodynamics. Russian Geology and Geophysics, 49: 254-271. [31]Safonova I Y.2009. Intraplate magmatism and oceanic plate stratigraphy of the Paleo-Asian and Paleo-Pacific Oceans from 600 to 140 Ma. Ore Geology Reviews, 35: 137-154. [32]Safonova I Y,Buslov M M,Simonov V A,Izokh A E,Komiya T,Kurganskaya E V,Ohno Т.2011. Geochemistry,petrogenesis and geodynamic origin of basalts from the Katun accretionary complex of Gorny Altay,south-western Siberia. Russian Geology and Geophysics, 52: 421-442. [33]Safonova I Y.2017. Juvenile versus recycled crust in the Central Asian Orogenic Belt: implications from ocean plate stratigraphy,blue schist belts and intra-oceanic arcs. Gondwana Research, 47: 6-27. [34]Sano H,Kanmera K.1991. Collapse of ancient oceanic reef complex—what happened during collision of Akiyoshi reef complex?sequence of collisional collapse and generation of collapse products. Journal of the Geological Society of Japan, 97: 631-644. [35]Santosh M.2010. A synopsis of recent conceptual models on supercontinent tectonics in relation to mantle dynamics,life evolution and surface environment. Journal of Geodynamics, 50: 116-133. [36]Stern C R.2011. Subduction erosion: rates,mechanisms,and its role in arcmagmatism and the evolution of the continental crust and mantle. Gondwana Research, 20: 284-308. [37]Utsunomiya A,Suzuki N,Ota T.2008. Preserved paleo-oceanic plateaus in accretionary complexes: implications for the contributions of the Pacific super plume to global environmental change. Gondwana Research, 14: 115-125. [38]Wakita K,Metcalfe I.2005. Ocean plate stratigraphy in East and Southeast Asia. Journal of Asia Earth Sciences, 24: 679-702. [39]Wang J X,Zhang K X,Jin J S, Song B W, Yu Y, Wang L J, Wang S D, Sun S.2020. Early Paleozoic ocean plate stratigraphy of the Beishan orogenic zone,NW China: implications for regional tectonic evolution. Acta Geologica Sinica(English Edition), 94: 1042-1059. [40]Yamazaki T,Okamura Y.1991. Subducting seamounts and deformation of overriding forearc wedges around Japan. Tectonophysics, 160: 1-4.
