The geophysical interpretation of Yandang Low Uplift and discussion on its genesis in the East China Sea Shelf Basin
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摘要: 通过对东海陆架盆地西部地震和重磁资料的综合地球物理解释,对雁荡低凸起展布形态进行了细致刻画,凸起呈NE方向不连续展布于瓯江凹陷和闽江凹陷之间,长约170 km、宽约15~50 km.地震资料揭示雁荡低凸起上广泛发育了侏罗纪与白垩纪地层,厚度约为500~1500 m,展布面积约5000 km2,局部缺失中生界地层.凸起两侧中生代盆地结构差异明显,西侧瓯江凹陷为典型的断陷盆地,东断西超、断裂发育,半地堑、掀斜断块等中生界构造样式发育;东侧闽江凹陷为坳陷型盆地,断裂、火成岩不发育,挤压背斜、断背斜、反转构造等中生界构造样式发育.自由空间重力异常图与剩余重力异常图上,凸起表现为一系列NE向团块状重力高值区,而磁力异常ΔT图上则表现为深部磁场强度低的特征,火成岩影响部位可见磁力高值异常.综合凸起及邻域重磁震、莫霍面深度等地质地球物理资料,认为雁荡低凸起为一元古界组成的古隆起,区别于东部的台北低凸起.同时,结合区域构造演化及沉积特征,推测侏罗纪时期雁荡低凸起与浙闽隆起区可能连为一体,晚白垩世近东西向伸展作用下浙闽隆起发生裂陷进而形成了雁荡低凸起.Abstract: Based on the geophysical interpretation of seismic, gravity and magnetic data of the western East China Sea Shelf Basin, this paper studied the distribution configuration of Yandang Low Uplift in detail and concluded that the uplift lied between Oujiang Sag and Minjiang Sag in a discontinuous NE-trending, about 170 km long and 15~50 km in width. There are widespread Jurassic and Cretaceous strata on the Yandang Low Uplift covering about 5000 km2 except some absence locally and the strata thickness is about 500~1500 m. Oujiang Sag distinctly differs from Minjiang Sag in the Mesozoic basin structure. The former is a typical faulted basin with "boundary fault in the east and overlap in the west" and well-developed faults. It also has well-developed Mesozoic half-grabens, tilted fault blocks. However, Minjiang Sag is a down-warped basin with less faults and igneous rock. Mesozoic compressional anticlines, faulted anticlines and inverted structures occur in large amounts. The uplift appears as a series of high value areas in NE-trending on free air gravity anomalies map and residual gravity anomalies map, while it appears as low magnetic anomaly areas in deep part on the ΔT magnetic anomalies map and there are high values of magnetic anomalies where igneous rocks exist. These geophysical features suggest that Yandang Low Uplift is a Proterozoic uplift which is different from Taipei low uplift. Meanwhile, this paper presumes that Yandang Low Uplift and Zhe-Min uplift may be joined in a single entity in Jurassic and divided into two parts in late Cretaceous according to the regional tectonic evolution and sedimentary characteristics.
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[1] Chen X H, Liu Z, Zhang Z X, et al. 2013. Deducing the East China Sea shelf basin by jointing gravity and seismic data. Progress in Geophys. (in Chinese), 28(3): 1596-1601.
[2] Feng X J, Zhang C Y, Wang C X, et a1. 2001. Mesozoic in the East China Sea Shelf and Taixinan Basin and its petroleum potential. China Offshore Oil and Gas (Geology) (in Chinese), 15(5): 306-310, 316.
[3] Feng X J, Cai D S, Wang C X, et al. 2003. The Meso-Cenozoic tectonic evolution in East China Sea Shelf Basin. China Offshore Oil and Gas (Geology) (in Chinese), 17(1): 33-37.
[4] Gao D Z. 1995. Density and magnetic of rocks in the East Sea shelf basin. Shanghai Geology (in Chinese), 54(2): 38-45.
[5] Gao D Z, Zhao J H, Bo Y L, et al. 2004. A profile study of gravitative-magnetic and seismic comprehensive survey in the East China Sea. Chinese J. Geophys. (in Chinese), 47(5): 853-861.
[6] Gao L. 2005. Mesozoic remnant basin characteristics and hydrocarbon exploration direction on East China Sea shelf. China Offshore Oil and Gas (in Chinese), 17(3): 148-152.
[7] Gong J M, Li G, Yang C S, et al. 2013. Hydrocarbon prospecting of Mesozoic Strata in Southern East China Sea shelf basin. Journal of Jilin University (Earth Science Edition) (in Chinese), 43(1): 20-27.
[8] Gong J M, Xu L M, Yang Y Q, et al. 2014. Discussion on Mesozoic hydrocarbon potential of southern East China Sea based on comparison between offshore and onshore areas. Global Geology (in Chinese), 33(1): 171-178.
[9] Han B, Zhang X H, Pei J X, et al. 2007. Characteristics of crust-mantle in East China sea and adjacent regions. Progress in Geophys. (in Chinese), 22(2): 376-382.
[10] Hao T Y, Xu Y, Xu Yi, et al. 2006. Some new understandings on deep structure in Yellow Sea and East China Sea. Chinese J. Geophys. (in Chinese), 49(2): 458-468.
[11] Jiang L. 2003. Exploration status and perspective of petroleum resources in East China Sea shelf basin. China Offshore Oil and Gas (Geology) (in Chinese), 17(1): 1-5.
[12] Li G, Gong J M, Yang C Q, et al. 2012. Stratigraphic features of the Mesozoic "Great East China Sea"—A new exploration field. Marine Geology and Quaternary Geology (in Chinese), 32(3): 97-104.
[13] Li J H, Zhang Y Q, Dong S W, et al. 2014. Cretaceous tectonic evolution of South China: A preliminary synthesis. Earth-Sci. Rev., 134: 98-136, doi: 10.106/j.earscirev.2014.03.008.
[14] Li S Z, Santosh M, Jahn B M. 2012a. Evolution of the Asian continent and its continental margins. Journal of Asian Earth Sciences, 47:1-4, doi:10.1016/j.jseaes.2012.02.001.
[15] Li S Z, Zhao G C, Dai L M, et al. 2012b. Mesozoic basins in eastern China and their bearing on the deconstruction of the North China Craton. Journal of Asian Earth Sciences, 47: 64-79, doi:10.1016/j.jseaes.2011.06.008.
[16] Li X W, Zhou X M. 1995. Late Mesozoic subduction zone of southeastern China. Geological Journal of China Universities (in Chinese), 5(2): 164-169.
[17] Liu J S, Liao Z T, Jia J Y, et al. 2003. The geological structure and tectonic evolution of the East China Sea Shelf Basin. Shanghai Geology (in Chinese), (3): 1-6.
[18] Shu L S, Zhou X M, Deng P, et al. 2009. Mesozoic tectonic evolution of the Southeast China Block: New insights from basin analysis. Journal of Asian Earth Sciences, 34(3): 376-391, doi:10.1016/j.jseaes.2008.06.004.
[19] Sun X M, Wang P J, Hao F J, et al. 2005. Space-time distribution features, migration regulation and genetic types of epicontinent of the East China. Journal of Jilin University (Earth Science Edition) (in Chinese), 35(5): 554-563.
[20] Suo Y H, Li S Z, Dai L M, et al. 2010. Division and characteristics of tectonic units of the East China Sea shelf basin. Marine Geology and Quaternary Geology (in Chinese), 30(6): 49-58.
[21] Suo Y H, Li S Z, Dai L M, et al. 2012. Cenozoic tectonic migration and basin evolution in East Asia and its continental margins. Acta Petrologica Sinica (in Chinese), 28(8): 2602-2618.
[22] Suo Y H, Li S Z, Zhao S J, et al. 2013. Continental margin basins in East Asia: tectonic implications of the Meso-Cenozoic East China Sea pull-apart basins. Geological Journal, doi:10.1002/gj.2535.
[23] Tang J. 2007. Study on the Mesozoic sedimentary strata distribution of East China and adjacent areas [Master's thesis] (in Chinese). Shanghai: Tongji University.
[24] Tao R M. 1994. Discussion on division of tectonic units in the southeastern East China Sea shelf basin. South China Petroleum Geology (in Chinese), (1): 62-67.
[25] Tian B, Li X Y, Pang G Y, et al. 2012. Sedimentary systems of the superimposed rift-subsidence basin: taking Lishui-Jiaojiang Sag of the East China Sea as an example. Acta Sedimentologica Sinica (in Chinese), 30(4): 696-705.
[26] Wan T F. 2011. The tectonics of China (in Chinese). Beijing: Geological Publishing House, 168-184.
[27] Wang G C. 1987. Formation and evolution of the East China Sea Basin. Acta Peirolet Sinica (in Chinese), 8(4): 18-25.
[28] Wang K D, Wang J P, Xu G Q, et al. 2000. The discovery and division of the Mesozoic Strata in the Southwest of Donghai shelf basin. Journal of Stratigraphy (in Chinese), 24(2): 129-131.
[29] Xu X H, Chen L L, Wang Q H. 2004. Analysis of Mesozoic geological characteristics and resource potential in the East China Sea shelf basin. Offshore Oil (in Chinese), 24(3): 1-7.
[30] Yang C Q, Yang C S, Li G, et al. 2012. Mesozoic tectonic evolution and prototype basin characters in the Southern East China Sea shelf basin. Marine Geology and Quaternary Geology (in Chinese), 32(3): 105-111.
[31] Yang C S, Li G, Yang C Q, et al. 2012. Temporal and spatial distribution of the igneous rocks in the East China Sea shelf basin and its adjacent regions. Marine Geology and Quaternary Geology (in Chinese), 32(3): 125-133.
[32] Yang J Y, Xu S Z, Yu H L, et al. 2008. Application of apparent density inversion method in the East China Sea and its adjacent area. Chinese J. Geophys. (in Chinese), 51(6): 1909-1916.
[33] Yang W D, Cui Z K, Zhang Y B. 2010. Geology and mineral resources of the East China Sea (in Chinese). Beijing: Marine Press, 390-405.
[34] Yang Y. 2010. Research on Mesozoic strata in the southern part of East China Sea by gravity and magnetic anomalies [Master's thesis] (in Chinese). Xi'an: Chang'an University.
[35] Yang Y Q, Li G, Dai C S. 2011. Characteristics of Mesozoic distribution and discussion on its favourable area in western depression zone of East China Sea shelf basin. Global Geology (in Chinese), 30(3): 396-403.
[36] Yin Y H, Zhang X H, Wen Z H, et al. 2008. The mapping methods and division of tectonics of the regional tectonic map in the Huanghai Sea and the East China Sea and adjacent regions. Acta Oceanologica Sinica (in Chinese), 30(6): 99-105.
[37] Zhang G W, Guo A L, Wang Y J, et al. 2013. Tectonics of South China Continent and its implications. Science China: Earth Sciences, 56(11): 1804-1828, doi:10.1007/s11430-013-4679-1.
[38] Zhang X H. 2008. Tectonic Geology in China Seas (in Chinese). Beijing: Ocean Press, 104-114.
[39] Zheng Q G, Zhou Z Y, Cai L G, et al. 2005. Meso-Cenozoic tectonic setting and evolution of East China Sea Shelf Basin. Oil and Gas Geology (in Chinese), 26(2): 197-201.
[40] Zhou Z Y, Gao J Y, Wu Z C, et al. 2013. Preliminary analyses of the characteristics of Moho undulation and crustal thinning in East China Sea. Journal of Marine Sciences (in Chinese), 31(1): 16-25.
[41] Zhu J J, Wang Q, Liang J S, et al. 2012. Cenozoic geological structure and tectonic evolution of southern East China Sea shelf basin. Natural Gas Geoscience (in Chinese), 23(2): 222-229.
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