The internal structure and evolution of the middle Diaoyudao Uplift in the East China Sea

doi:10.3969/j.issn.1001-909X.2020.04.001

Abstract

Abstract: Due to the lack of geological and geophysical data of the Diaoyudao Uplift, the previous studies on this area are unsystematic, so there are many controversies about its tectonic evolution. Based on gravity, magnetic, and multichannel seismic data, the tectonic and sedimentary characteristics of the middle Diaoyudao Uplift were analyzed, which located to the east of the Xihu Depression, East China Sea Basin. The evolution model of the middle Diaoyudao Uplift was further refined. More residual sags are found in the north than in the south of the middle Diaoyudao Uplift. Accordingly, the middle Diaoyudao Uplift can be divided into the north and south segments. The boundary of the two segments is on the extended trace of the Zhoushan-Guotou Fault. In addition, magmatic intrusions are confined below the T20 unconformity in the west, whereas a basement pinnacle caused by magmatic activity exists in the east. It is found that the gradient zone of gravity anomaly corresponds exactly to the western edge of the basement pinnacle. Taking the west edge of the basement pinnacle as the boundary, the middle Diaoyudao Uplift can be divided into two parts from west to east. And the western zone can be further divided into two subzones, including part Ⅰ with magnetic rocks and part Ⅱ with residual sags. The western part of the middle Diaoyudao Uplift is from the strong tectonic and magmatic deformation of the eastern Xihu Depression, whereas the east part retained the original Diaoyudao Uplift. The comprehensive analysis of above features showed that the present-day middle Diaoyudao Uplift was formed by many episodes of tectonic events and magmatic activities around an ancient uplift.

Key words: the middle Diaoyudao Uplift, magmatism, inner divisions, tectonic evolution

CLC Number:

P736.1

LI Kedi, LI Chunfeng, YAO Zewei, TAO Tiansheng. The internal structure and evolution of the middle Diaoyudao Uplift in the East China Sea[J]. Journal of Marine Sciences, 2020, 38(4): 1-15.

References

[1] SIBUET J C, LETOUZEY J, BARBIER F, et al. Back arc extension in the Okinawa Trough[J]. Journal of Geophysical Research Solid Earth, 1987, 92(B13): 14041.
[2] SIBUET J C, DEFFONTAINES B, HSU S K, et al. Okinawa trough backarc basin: Early tectonic and magmatic evolution[J]. Journal of Geophysical Research Solid Earth, 1998, 103(B12): 30245-30267.
[3] 赵金海.东海中、新生代盆地成因机制和演化(上)[J].海洋石油,2004,24(4):1-10.
ZHAO Jinhai. The forming factors and evolvement of the Mesozoic and Cenozoic basin in the East China Sea[J]. Offshore Oil, 2004, 24(4): 1-10.
[4] ZHU Weilin, ZHONG Kai, FU Xiaowei, et al. The formation and evolution of the East China Sea Shelf Basin: A new view[J]. Earth-Science Reviews, 2019, 190: 89-111.
[5] 刘金水,许怀智,蒋一鸣,等.东海盆地中、新生代盆架结构与构造演化[J].地质学报,2020,94(3):675-691.
LIU Jinshui, XU Huaizhi, JIANG Yiming, et al. Mesozoic and Cenozoic basin structure and tectonic evolution in the East China Sea basin[J]. Acta Geologica Sinica, 2020, 94(3): 675-691.
[6] CUKUR D, HOROZAL S, KIM D C, et al. Seismic stratigraphy and structural analysis of the northern East China Sea Shelf Basin interpreted from multi-channel seismic reflection data and cross-section restoration[J]. Marine and Petroleum Geology, 2011, 28(5): 1003-1022.
[7] 王鹏,赵志刚,张功成,等.东海盆地钓鱼岛隆褶带构造演化分析及对西湖凹陷油气勘探的意义[J].地质科技情报,2011,30(4):65-72.
WANG Peng, ZHAO Zhigang, ZHANG Gongcheng, et al. Analysis on structural evolution in Diaoyu Islands Folded-Uplift Belt, East China Sea Basin and its impact on the hydrocarbon exploration in Xihu Sag[J]. Geological Science and Technology Information, 2011, 30(4): 65-72.
[8] 李学伦,刘保华,林振宏,等.东海陆架外缘隆褶带的形成与构造演化[J].海洋学报(中文版),1997,19(5):76-82.
LI Xuelun, LIU Baohua, LIN Zhenhong, et al. Formation and tectonic evolution of uplift fold belt on the outer margin of the East China Sea[J]. Acta Oceanologica Sinica, 1997, 19(5): 76-82.
[9] 巩兴会,陈琳琳,李昆,等.东海陆架盆地西湖凹陷东部边缘结构解释及地质意义[J].吉林大学学报(地球科学版),2019,49(1):154-164.
GONG Xinghui, CHEN Linin, LI Kun, et al. Structure types and its geological significance of eastern edge of Xihu Sag in the East China Shelf Basin[J]. Journal of Jilin University(Earth Science Edition), 2019, 49(1): 154-164.
[10] 蒋一鸣,何新建,唐贤君,等.钓鱼岛隆褶带物质构成及东海西湖凹陷原型盆地东边界再认识[J].地球科学,2019,44(3):773-783.
JIANG Yiming, HE Xinjian, TANG Xianjun, et al. Material composition of Diaoyu Islands Folded Zone and reanalysis of eastern boundary of prototype basin of Xihu Sag in East China Sea[J]. Earth Science, 2019, 44(3): 773-783.
[11] SUO Yanhui, LI Sanzhong, JIN Chong, et al. Eastward tectonic migration and transition of the Jurassic-Cretaceous Andean-type continental margin along Southeast China[J]. Earth-Science Reviews, 2019, 196: 102884.
[12] DING Weiwei, LI Jiabiao, WU Zhaocai, et al. Late Mesozoic transition from Andean-type to Western Pacific-type of the East China continental margin—Is the East China Sea basement an allochthonous terrain?[J]. Geological Journal, 2018, 53(5): 1994-2002.
[13] 蒋一鸣,何新建,张绍亮.东海陆架盆地“反转-改造”构造迁移演化特征——以西湖凹陷边缘构造为例[J].长江大学学报(自科版),2016,13(26):1-8.
JIANG Yiming, HE Xinjian, ZHANG Shaoliang. The characteristics of “inverse-transform” tectonic migration evolution of the East China Sea Shelf Basin[J]. Journal of Yangtze University(Natural Science Edition), 2016, 13(26): 1-8.
[14] 李祥权,刘金水,陆永潮,等.东海陆架盆地西湖凹陷花港组原型盆地性质厘定[J].地球科学,2018,43(2):502-513.
LI Xiangquan, LIU Jinshui, LU Yongchao, et al. Prototype basin characterization of Huagang Formation of Xihu Depression, East China Sea Shelf Basin[J]. Earth Science, 2018, 43(2): 502-513.
[15] HSU S K, SIBUET J C, SHYU C T. Magnetic inversion in the East China Sea and Okinawa Trough: Tectonic implications[J]. Tectonophysics, 2001, 333(1): 111-122.
[16] SHANG Luning, ZHANG Xunhua, JIA Yonggang, et al. Late Cenozoic evolution of the East China continental margin: Insights from seismic, gravity, and magnetic analyses[J]. Tectonophysics, 2017, 698: 1-15.
[17] YAO Zewei, LI Chunfeng, HE Guangyu, et al. Cenozoic sill intrusion in the central and southern East China Sea Shelf Basin[J]. Marine and Petroleum Geology, 2020, 119(7): 104465.
[18] FANG Penggao, DING Weiwei, LIN Xiubin, et al. Neogene subsidence pattern in the multi-episodic extension systems: Insights from backstripping modelling of the Okinawa Trough[J]. Marine and Petroleum Geology, 2020, 111: 662-675.
[19] 王超,唐贤君,蒋一鸣,等.西湖凹陷天台斜坡带北部构造变换带特征及油气地质意义[J].海洋地质与第四纪地质,2020,40(6):93-105.
WANG Chao, TANG Xianjun, JIANG Yiming, et al. Characteristics of the structural transfer zone of northern Tiantai slope in Xihu Sag of the East China Sea Basin and their petroleum geological significances[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 93-105.
[20] 郑求根,周祖翼,蔡立国,等.东海陆架盆地中新生代构造背景及演化[J].石油与天然气地质,2005,26(2):197-201.
ZHENG Qiugen, ZHOU Zuyi, CAI Liguo, et al. Meso-Cenozoic tectonic setting and evolution of East China Sea shelf basin[J]. Oli & Gas Geology, 2005, 26(2): 197-201.
[21] 杨长清,杨传胜,李刚,等.东海陆架盆地南部中生代构造演化与原型盆地性质[J].海洋地质与第四纪地质,2012,32(3):105-111.
YANG Changqing, YANG Chuansheng, LI Gang, et al. Mesozoic tectonic evolution and prototype basin characters in the southern East China Sea Shelf Basin[J]. Marine Geology & Quaternary Geology, 2012, 32(3): 105-111.
[22] 赵志刚,王鹏,祁鹏,等.东海盆地形成的区域地质背景与构造演化特征[J].地球科学,2016,41(3):546-554.
ZHAO Zhigang, WANG Peng, QI Peng, et al. Regional background and tectonic evolution of East China Sea Basin[J]. Earth Science, 2016, 41(3): 546-554.
[23] 周新华,鄂莫岚,张剑波.东海早第三纪玄武岩的发现及其区域地幔地球化学成因意义[J].岩石学报,1992,8(4):395-398.
ZHOU Xinhua, E Molan, ZHANG Jianbo. Early tertiary basalt in East China Sea Basin and its implications to regional mantle geochemistry[J]. Acta Petrologica Sinica, 1992, 8(4): 395-398.
[24] 尚鲁宁.冲绳海槽构造地质特征及形成演化研究[D].青岛:中国海洋大学,2014.
SHANG Luning. Tectonics and evolution of the Okinawa Trough[D]. Qingdao: Ocean University of China, 2014.
[25] GUNGOR A, LEE G H, KIM H J, et al. Structural characteristics of the northern Okinawa Trough and adjacent areas from regional seismic reflection data: Geologic and tectonic implications[J]. Tectonophysics, 2012, 522-523(3): 198-207.
[26] 李桂群,李学伦.东海陆架外缘隆起带地质构造特征[J].青岛海洋大学学报,1995,25(2):199-205.
LI Guiqun, LI Xuelun. Geological tectonic characteristics of the outer margin upwarped zone of the East China Sea Shelf[J]. Journal of Ocean University of Qingdao, 1995, 25(2): 199-205.
[27] 尚鲁宁,张勇,张训华,等.东海陆架外缘区构造特征及其成因机制[J].海洋与湖沼,2018,49(6):1178-1189.
SHANG Luning, ZHANG Yong, ZHANG Xunhua, et al. Tectonic structure of the outer shelf of the East China Sea and the formation mechanism[J]. Oceanologia et Limnologia Sinica, 2018, 49(6): 1178-1189.
[28] 朱立新.西湖凹陷新生代火成岩发育特征及区域背景分析[J].海洋石油,2016,36(3):1-7.
ZHU Lixin. Characteristics and regional background of Cenozoic igneous rocks in Xihu Sag[J]. Offshore Oil, 2016, 36(3): 1-7.
[29] KONG F C, LAWVER L A, LEE T Y. Evolution of the southern Taiwan-Sinzi Folded Zone and opening of the southern Okinawa trough[J]. Journal of Asian Earth Sciences, 2000, 18(3): 325-341.
[30] SANDWELL D T, MÜLLER R D, SMITH W H F, et al. New global marine gravity model from CryoSat-2 and Jason-1 reveals buried tectonic structure[J]. Science, 2014, 346(6205): 65-67.
[31] Geological Survey of Japan and Coordinating Committee for Coastal and Offshore Geoscience Programmes in East and Southeast Asia (CCOP). Magnetic anomaly map of East Asia 1 4 000 000[Z/CD]. 1996.
[32] 周心怀,蒋一鸣,唐贤君.西湖凹陷成盆背景、原型盆地演化及勘探启示[J].中国海上油气,2019,31(3):1-10.
ZHOU Xinhuai, JIANG Yiming, TANG Xianjun. Tectonic setting, prototype basin evolution and exploration enlightenment of Xihu sag in East China Sea basin[J]. China Offshore Oil and Gas, 2019, 31(3): 1-10.
[33] LI Chunfeng, ZHOU Zuyi, GE Heping, et al. Rifting process of the Xihu Depression, East China Sea Basin[J]. Tectonophysics, 2009, 472(1-4): 135-147.
[34] ROEST W R, VERHOEF J, PILKINGTON M. Magnetic interpretation using the 3-D analytic signal[J]. Geophysics, 1992, 57(1): 116-125.
[35] 柴利根.论鱼山-久米断裂带性质及其对东海地质构造的控制作用[J].石油与天然气地质,1986(2):107-115.
CHAI Ligen. The nature of Yushan-kume fault belt and its control over East China Sea[J]. Oil & Gas Geology, 1986(2): 107-115.
[36] 张绍亮,张建培,唐贤君,等.东海西湖凹陷断裂系统几何学特征及其成因机制[J].海洋地质与第四纪地质,2014,34(1):87-94.
ZHANG Shaoliang, ZHANG Jianpei, TANG Xianjun, et al. Geometry characterstic of the fault system in Xihu Sag in East China Sea and its formation mechanism[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 87-94.
[37] 刘光鼎.中国海区及邻域地质地球物理特征[M].北京:科学出版社,1992.
LIU Guangding. Geological and geophysical characteristics of China's sea area and its adjacent areas[M]. Beijing: Science Press, 1992.
[38] 刘建军,陈开远,史忠生,等. 东海陆架盆地西湖凹陷下第三系物源分析[J].科技进步与对策,2003(S1):241-242.
LIU Jianjun, CHEN Kaiyuan, SHI Zhongsheng, et al. Paleogene source analysis of Xihu Sag in East China Sea Shelf Basin[J]. Science & Technology Progress and Policy, 2003(S1): 241-242.
[39] 侯方辉,张训华,李刚,等.从被动陆缘到主动陆缘——东海陆架盆地中生代构造体制转换的盆地记录[J].石油地球物理勘探,2015,50(5):980-990.
HOU Fanghui, ZHANG Xunhua, LI Gang, et al. From passive continental margin to active continental margin: basin recordings of Mesozoic tectonic regime transition of the East China Sea Shelf Basin[J]. Oil Geophysical Prospecting, 2015, 50(5): 980-990.
[40] LI Zhengxiang, LI Xianhua. Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China: A flat-slab subduction model[J]. Geology, 2007, 35(2): 179-182.
[41] 杨传胜,李刚,杨长清,等.东海陆架盆地及其邻域岩浆岩时空分布特征[J].海洋地质与第四纪地质,2012,32(3):125-133.
YANG Chuansheng, LI Gang, YANG Changqing, et al. Temporal and spatial distribution of the igneous rocks in the East China Sea Shelf Basin and its adjacent regions[J]. Marine Geology & Quaternary Geology, 2012, 32(3): 125-133.
[42] YANG Changqing, HAN Baofu, YANG Chuansheng, et al. Mesozoic basin evolution of the East China Sea Shelf and tectonic system transition in Southeast China[J]. Geological Journal, 2018, 55(1): 239-252.
[43] 包汉勇,郭战峰,张罗磊,等.太平洋板块形成以来的中国东部构造动力学背景[J].地球科学进展,2013,28(3):337-346.
BAO Hanyong, GUO Zhanfeng, ZHANG Luolei, et al. Tectonic dynamics of eastern China since the formation of the Pacific Plate[J]. Advances in Earth Science, 2013, 28(3): 337-346.
[44] NORTHRUP C J, ROYDEN L H, BURCHFIEL B C. Motion of the Pacific plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia[J]. Geology, 1995, 23(8): 719.
[45] 李三忠,余珊,赵淑娟,等.东亚大陆边缘的板块重建与构造转换[J].海洋地质与第四纪地质,2013,33(3):65-94.
LI Sanzhong, YU Shan, ZHAO Shujuan, et al. Tectonic transition and plate reconstructions of the east Asian continental margin[J]. Marine Geology & Quaternary Geology, 2013, 33(3): 65-94.
[46] 索艳慧,李三忠,曹现志,等.中国东部中新生代反转构造及其记录的大洋板块俯冲过程[J].地学前缘,2017,24(4):249-267.
SUO Yanhui, LI Sanzhong, CAO Xianzhi, et al. Mesozoic-Cenozoic inversion tectonic of East China and its implications for the subduction process of the oceanic plate[J]. Earth Science Frontiers, 2017, 24(4): 249-267.
[47] 宋陶然,李春峰.由高密度磁异常测量数据分析南海海盆的扩张年龄与扩张模式[J].地球物理学进展,2012,27(4):1432-1442.
SONG Taoran, LI Chunfeng. The opening ages and mode of the South China Sea estimated from high-density magnetic tracks[J]. Progress in Geophysics, 2012, 27(4): 1432-1442.
[48] 秘丛永.西湖凹陷中央反转带和平湖斜坡带断裂特征及演化[D].青岛:中国海洋大学,2015.
MI Congyong. The fault characteristics and evolution of central inversion tectonic belt and Pinghu Slope in Xihu sag[D]. Qingdao: Ocean University of China, 2015.
[49] 杨文达,崔征科,张异彪.东海地质与矿产[M].北京:海洋出版社,2010.
YANG Wenda, CUI Zhengke, ZHANG Yibiao. Geology and minerals of the East China Sea[M]. Beijing: China Ocean Press, 2010.