APPROACH OF GEOLOGICAL TECTONIC MAPPING OF OCEANIC PLATE IN SUBDUCTION ACCRETIONARY COMPLEX ZONE
ZHANG Ke-xin1,2,3, ZHANG Jin4, PAN Gui-tang5, LIU Yong4, HE Wei-hong2,3, XU Ya-dong2,3, SONG Bo-wen1, ZHANG Xiong-hua3
1. Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China; 2. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China; 3. School of Earth Sciences, China University of Geosciences, Wuhan 430074, China; 4. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China; 5. Chengdu Center of China Geological Survey, Chengdu 610082, China
Abstract:The quality of geological mapping lies in reasonable determination of mapping units of different levels. The compositions of subduction accretionary complex zone are mainly derived from the structure-formation of oceanic lithosphere in ocean basin under various tectonic environments, including oceanic ridge formation (ophiolite), abyssal plain formation, oceanic island-seamount formation, intra-oceanic arc formation, trench formation and high-ultrahigh pressure rock formation. Besides, there are also rifted block formation, high-ultrahigh pressure rock formation, continental margin magmatic arc formation and wedge-top basin formation derived from continental lithosphere which are mixed into the subduction accretionary complex zone. Therefore, it is basic to identify and determine the geological formations of different sources for mapping unit division and compilation. Based on the scientific objective of distinguishing different material sources in subduction accretionary complex zone, the mapping units are divided into three levels:subduction accretionary complex zone(first-level unit), slice(second-level unit) and rock block and matrix (third-level unit) which are divided and named with the requirements for code, coloring and lithologic pattern. The paper briefly describes the requirements of graphic expression of structural deformation in subduction accretionary complex zone, and emphasizes that the structural deformations during subduction and collision are the two major deformation periods, thus the mapping must be reasonable and accurate.
李廷栋,肖庆辉,潘桂棠,等.关于发展洋板块地质学的思考[J].地球科学, 2019, 44(5):1441-1451. Li T D, Xiao Q H, Pan G T, et al. A consideration about the development of ocean plate geology[J]. Earth Science, 2019,44(5):1441-1451.
[2]
张克信,童金南,赖旭龙,等.地层单位与全球界线层型:概念、术语、有关规定与研究实例[J].地质科技情报, 2012, 31(5):23-42. Zhang K X, Tong J N, Lai X L, et al. Stratigraphic unit and GSSP:Concept, nomenclature, regulation and example[J]. Geological Science and Technology Information, 2012, 31(5):23-42.
[3]
龚一鸣,张克信.地层学基础与前沿[M]. 2版.武汉:中国地质大学出版社, 2016. Gong Y M, Zhang K X. Stratigraphic fundamentals and frontiers[M]. 2nd ed. Wuhan:China University of Geosciences Press, 2016.
[4]
刘勇,李廷栋,肖庆辉,等.洋板块地质研究进展[J].地学前缘, 2022, 29(2):79-93. Liu Y, Li T D, Xiao Q H, et al. Progress in geological study of oceanic plates[J]. Earth Science Frontiers, 2022, 29(2):79-93.
[5]
潘桂棠,肖庆辉,张克信,等.大陆中洋壳俯冲增生杂岩带特征与识别的重大科学意义[J].地球科学, 2019, 44(5):1544-1561. Pan G T, Xiao Q H, Zhang K X, et al. Recognition of the oceanic subduction-accretion zones from the orogenic belt in continents and its important scientific significance[J]. Earth Science, 2019,44(5):1544-1561.
[6]
Isozaki Y, Maruyama S, Furuoka F. Accreted oceanic materials in Japan[J]. Tectonophysics, 1990, 181(1/4):179-205.
[7]
张克信,殷鸿福,朱云海,等.造山带混杂岩区地质填图理论、方法与实践——以东昆仑造山带为例[M].武汉:中国地质大学出版社, 2001. Zhang K X, Yin H F, Zhu Y H, et al. Geological survey theory, method and practice of mélange zone in Orogenic belt[M]. Wuhan:China University of Geosciences Press, 2001.(in Chinese)
[8]
张克信,冯庆来,宋博文,等.造山带非史密斯地层[J].地学前缘, 2014, 21(2):36-47. Zhang K X, Feng Q L, Song B W, et al. Non-smithian strata in the orogen[J]. Earth Science Frontiers, 2014, 21(2):36-47.
[9]
张克信,李仰春,王丽君,等.造山带混杂岩及相关术语[J].地质通报, 2020, 39(6):765-782. Zhang K X, Li Y C, Wang L J, et al. The divisions of mélange in the orogenic belt and its associated terminologies[J]. Geological Bulletin of China,2020,39(6):765-782.
[10]
Kusky T M, Windley B F, Safonova I, et al. Recognition of ocean plate stratigraphy in accretionary orogens through Earth history:A record of 3.8 billion years of sea floor spreading, subduction, and accretion[J]. Gondwana Research,2013,24(2):501-547.
[11]
潘桂棠,肖庆辉,陆松年,等.大地构造相的定义、划分、特征及其鉴别标志[J].地质通报, 2008, 27(10):1613-1637. Pan G T, Xiao Q H, Lu S N, et al. Definition, classification, characteristics and diagnostic indications of tectonic facies[J]. Geological Bulletin of China, 2008, 27(10):1613-1637.
[12]
潘桂棠,肖庆辉,尹福光,等.中国大地质构造图(1:2500000)说明书[M].北京:地质出版社, 2016. Pan G T, Xiao Q H, Yin F G, et al. Explanatory notes to the tectonic map of China (1:2500000)[M]. Beijing:Geological Publishing House, 2016.(in Chinese)
[13]
潘桂棠,肖庆辉,尹福光,等.中国大地构造[M].北京:地质出版社, 2017. Pan G T, Xiao Q H, Yin F G, et al. Tectonics of China[M]. Beijing:Geological Publishing House, 2017.(in Chinese)
[14]
张克信,何卫红,徐亚东,等.沉积大地构造相划分与鉴别[J].地球科学——中国地质大学学报, 2014, 39(8):915-928. Zhang K X, He W H, Xu Y D, et al. Subdivision and identification of sedimentary tectonic facies[J]. Earth Science-Journal of China University of Geosciences, 2014,39(8):915-928.
[15]
张克信.中国沉积大地构造图(1:2500000)[M].北京:地质出版社, 2015. Zhang K X. Sedimentary tectonic map of China (1:2500000)[M]. Beijing:Geological Publishing House, 2015.
[16]
王涛,裴先治,胡能高,等.一种特殊类型的变质火山-沉积岩系及其单位划分问题[C]//陈克强,汤家富.构造地层单位研究.武汉:中国地质大学出版社, 1995. Wang T, Pei X Z, Hu N G, et al. A special kind of metavolcano-sedimentary rock series and the classification of its units[C]//Chen K Q, Tang J F. The study of tectono-stratigraphy units. Wuhan:China University of Geosciences Press, 1995.
[17]
Leggett J K, McKerrow W S, Eales M H. The southern uplands of Scotland:A Lower Palaeozoic accretionary prism[J]. Journal of the Geological Society, 1979, 136(6):755-770.
[18]
Sawaki Y, Shibuya T, Kawai T, et al. Imbricated ocean-plate stratigraphy and U-Pb zircon ages from tuff beds in cherts in the Ballantrae complex, SW Scotland[J]. GSA Bulletin, 2010, 122(3/4):454-464.
[19]
Wang L J, Zhang K X, He W H, et al. An Early Paleozoic tectonic mélange at the western margin of west Cathaysia:Constraints from organic-walled microfossils[J]. Acta Geologica Sinica (English Edition), 2020, 94(4):1060-1070.
[20]
Wang L J, Zhang K X, Lin S F, et al. Origin and age of the Shenshan tectonic mélange in the Jiangshan-Shaoxing-Pingxiang fault and late Early Paleozoic juxtaposition of the Yangtze block and the west Cathaysia terrane, South China[J]. GSA Bulletin, 2022, 134(1/2):113-129.
[21]
Wakita K. Mappable features of mélanges derived from ocean plate stratigraphy in the Jurassic accretionary complexes of Mino and Chichibu terranes in southwest Japan[J]. Tectonophysics, 2012, 568-569:74-85.
[22]
Sano H, Kanmera K. Collapse of ancient oceanic reef complex-What happened during collision of Akiyoshi reef complex?Sequence of collisional collapse and generation of collapse products[J]. Journal-Geological Society of Japan, 1991, 97(8):631-644.
[23]
张克信,何卫红,徐亚东,等.中国洋板块地层分布及构造演化[J].地学前缘, 2016, 23(6):24-30. Zhang K X, He W H, Xu Y D, et al. Palaeogeographic distribution and tectonic evolution of OPS in China[J]. Earth Science Frontiers, 2016,23(6):24-30.
[24]
中华人民共和国国土资源部. GB/T958-2015区域地质图图例[S].北京:中国标准出版社, 2015. Ministry of Land and Resources of the People's Republic of China. GB/T958-2015 Geological legends used for regional geological maps[S]. Beijing:China Standards Press, 2015.
[25]
全国地层委员会《中国地层表》编委会.中国地层表(2014版)[M].北京:地质出版社, 2014. The Editorial Committee of National Commission Stratigraphy of China (The Stratigraphic Chart of China). The stratigraphic chart of China[M]. Beijing:Geological Publishing House, 2014.(in Chinese)
[26]
樊隽轩,李超,侯旭东.国际年代地层表(2018/08版)[J].地层学杂志, 2018, 42(4):365-370. Fan J X, Li C, Hou X D. International chronostratigraphic chart (v 2018/08)[J]. Journal of Stratigraphy, 2018, 42(4):365-370.
[27]
Maxwell J C. Anatomy of an orogen[J]. GSA Bulletin, 1974, 85(8):1195-1204.
[28]
Blake M C Jr, Jayko A S, McLaughlin R J, et al. Metamorphic and tectonic evolution of the Franciscan complex, northern California[C]//Ernst W G. Metamorphism and crustal evolution of the western United States:Rubey Volume VII:Englewood Cliffs. New Jersey:Prentice-Hall, 1988:1035-1060.
[29]
Wakabayashi J. Nappes, tectonics of oblique plate convergence, andmetamorphic evolution related to 140 million years of continuous subduction, Franciscan complex, California[J]. The Journal of Geology, 1992, 100(1):19-40.
[30]
Wakabayashi J. Subduction and the rock record:Concepts developedin the Franciscan complex, California[C]//Moores E M, Sloan D, Stout D L. Classic cordilleran concepts:A view from California. Boulder:Geological Society of America, 1999:123-133.
[31]
Wakabayashi J, Dilek Y. Mélanges:Processes of formation and societal significance[M]. Geological Society of America, 2011.
[32]
张进,曲军峰,赵衡,等.俯冲增生杂岩带变形特征、成因机制及与后期变形的区别[J].地学前缘, 2022, 29(2):56-78,doi:10.13745/j.esf.sf.2022.2.4. Zhang J, Qu J F, Zhao H, et al. Deformation in subduction-accretionary complex belts:Characteristics, mechanism and differentiation from late-stage event[J]. Earth Science Frontiers, 2022, 29(2):56-78.
[33]
殷鸿福,张克信.中华人民共和国区域地质调查报告——冬给措纳湖幅(I47C001002)[M].武汉:中国地质大学出版社, 2003. Yin H F, Zhang K X. The People's Republic of China regional geological report:Donggi Conag Hu Sheet (I47C001002)[M]. Wuhan:China University of Geosciences Press, 2003.(in Chinese)