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Discovery and significance of Lizifang metamorphic core complex in Zhuanghe area of southern Liaoning |
ZHONG Mishan1, 2, ZHANG Guoren2, WU Zijie2, 3, GAO Fuliang2, MA Ningning4, PAN Yuqi2, GAO Yongzhao2 |
1. College of Earth Sciences, Jilin University, Changchun 130061, China; 2. Liaoning Provincial Institute of Geological Exploration LLC, Dalian 116100, China; 3. School of Geosciences, China University of Petroleum(East China),Qingdao 266580, China; 4. Shandong Institute of Geological Surveying and Mapping, Jinan 250000, China |
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Abstract On the basis of the previous regional geological survey, based on the macroscopic and microscopic structural survey, combined with the comprehensive analysis of the regional magmatic activity and dating data, the authors in this paper revealed that there is another metamorphic core complex structure in Lizifang area of Southern Liaoning, namely Lizifang metamorphic core complex. A typical three-layer structure and five parts exist in the core complex, which are the footwall composed of Neo-archean metamorphic plutonic rocks and mesozoic granite intrusive rocks, the detachment fault zone composed of different levels of tectonic rocks, and the upper plate composed of Precambrian sedimentary cap and Cretaceous extensional basin. Lizifang metamorphic core complex formed in the Early Cretaceous Epoch, and the upper plate moved from NWW to SEE relaive to the footwall, which was similar with Jinzhou metamorphic core complex and Wanfu metamorphic core complex in geometry, kinematics polarity and formation time, indicating the same dynamic background. The determination of the metamorphic core complex may provide a basis for the late Mesozoic lithospheric thinning process and the mechanical and rheological properties of the lithosphere in the east of North China Craton. At the same time, the metamorphic core complex is closely related to the mineralization of gold deposits. So the detachment fault zone of Lizifang metamorphic core complex can serve as the key work area for further gold exploration, which may possess large mineralization potential.
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Received: 07 April 2020
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[1] 杨中柱,孟庆成,冮江,等.辽南变质核杂岩构造[J].辽宁地质,1996(4):241-250. [2] 刘俊来,关会梅,纪沫,等.华北晚中生代变质核杂岩构造及其对岩石圈减薄机制的约束[J].自然科学进展,2006,16(1):21-26. [3] 林伟,王清晨,王军,等.辽东半岛晚中生代伸展构造——华北克拉通破坏的地壳响应[J].中国科学:地球科学,2011,41(5):638-653. [4] 关会梅,刘俊来,纪沫,等.辽宁南部万福变质核杂岩的发现及其区域构造意义[J].地学前缘,2008,15(3):199-208. [5] 刘俊来,纪沫,申亮,等.辽东半岛早白垩世伸展构造组合、形成时代及区域构造内涵[J].中国科学:地球科学,2011,41(5):618-637. [6] 李建波,鲁勇花,蒋振频.辽南万福变质核杂岩韧性剪切带的应变与剪切作用类型[J].东华理工大学学报(自然科学版),2012,35(3):238-245. [7] 刘俊来,纪沫,夏浩然,等.华北克拉通晚中生代壳-幔拆离作用:岩石流变学约束[J].岩石学报,2009,25(8):1819-1829. [8] 杨中柱. 辽南印支期伸展构造研究[D].北京:中国地质大学(北京),2001:1-37. [9] 申亮. 辽东黄花甸—大营子伸展构造及其区域构造意义[D].北京:中国地质大学(北京),2009:1-65. [10] 申亮,刘俊来,胡玲,等.辽东半岛大营子拆离断层系及其区域构造意义[J].中国科学:地球科学,2011,41(4):437-451. [11] 申亮. 华北克拉通东部晚中生代构造体制转换——以辽东半岛为例[D].北京:中国地质大学(北京),2013. [12] 纪沫. 辽南变质核杂岩晚中生代构造岩浆关系[D].北京:中国地质大学(北京),2007. [13] 纪沫,刘俊来,胡玲,等.辽南变质核杂岩饮马湾山和赵房岩体锆石SHRIMP U-Pb年龄及其地质意义[J].岩石学报,2009,25(1):173-181. [14] 郑亚东,曾令森,李健波,等.辽南中生代造山期缩短滑脱与晚造山伸展拆离构造[J].地质科学,2009,44(3):811-824. [15] 林伟,王军,刘飞,等.华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论[J].岩石学报,2013,29(5):1791-1810. [16] 张国仁,杨中柱,仲米山,等.辽宁变质核杂岩及控矿规律研究[R].大连:辽宁省地质勘查院有限责任公司,2019. [17] 王启伟,孙厚江,张少华,等.中华人民共和国大营镇等四幅1∶5万区域地质调查报告[R].大连:辽宁省区域地质调查队,1996. [18] 陈树良,曲洪祥,杨中柱,等.中华人民共和国丹东市等两幅1∶25万区域地质调查报告[R].大连:辽宁省区域地质调查队,2003. [19] 吴福元,杨进辉,柳小明.辽东半岛中生代花岗质岩浆作用的年代学格架[J].高校地质学报,2005,11(3):305-317. [20] Wu F Y,Lin J Q,Wilde S A,et al.Nature and significance of the Early Cretaceous giant igneous event in Eastern China[J].Earth Planet Sci Lett,2005,233(1/2):103-119. [21] 许志琴,李海兵,王宗秀,等.辽南地壳的收缩作用及伸展作用[J].地质论评,1991,37(3):193-202. [22] Liu J L,Davis G A,Lin Z Y,et al.The Liaonan metamorphic core complex,southeastern Liaoning Province,North China:a likely contributor to Cretaceous rotation of Eastern Liaoning, Korea and contiguous areas[J].Tectonophysics,2005,407(1/2):65-80. [23] Lin W,Faure M,Monié P,et al.Polyphase Mesozoic tectonics in the eastern part of the North China Block:insights from the eastern Liaoning Peninsula massif (NE China)[C]//Mesozoic Sub-Continental Lithospheric Thinning Under Eastern Asia.Geological Society,London,Special Publications,2007,280:153-169. [24] Lin W,Faure M,Monié P,et al.Mesozoic extensional tectonics in Eastern Asia:the south Liaodong Peninsula metamorphic core complex (NE China)[J].The Journal of Geology,2008,116(2):134-154. [25] Yang J H,Wu F Y,Chung S L,et al.Rapid exhumation and cooling of the Liaonan metamorphic core complex:inferences from 40Ar/39Ar thermochronology and implications for Late Mesozoic extension in the eastern North China Craton[J].GSA Bulletin,2007,119(11/12):1405-l414. [26] Wang H Z,Mo X X.An outline of the tectonic evolution of Chi-na[J].Episodes,1995,18(1/2):6-16. [27] 翟明国,孟庆任,刘建明,等.华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨[J].地学前缘,2004,11(3):285-297. [28] 赵越,徐刚,张拴宏,等.燕山运动与东亚构造体制的转变[J].地学前缘,2004,11(3):319-328. [29] 许文良,王枫,裴福萍,等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报,2013,29(2):339-353. [30] Compston W,Williams I S,Kirschvink J L,et al.Zircon U-Pb ages for the Early Cambrian time-scale[J].J Geol Soc,1992,149(2):171-184. [31] 黎彤,袁怀雨.大洋岩石圈和大陆岩石圈的元素丰度[J].地球化学,2011,40(1):1-5. [32] 宋明春,伊丕厚,崔书学,等.“焦家式”金矿成矿理论[J].矿床地质,2012,31(增刊1):783-784. [33] 孟宪刚. 辽西医巫闾山北段中生代构造格架及其对金矿形成富集与分布的控制作用[D].北京:中国地质大学(北京),2003. [34] 仲米山,张国仁,杨中柱,等.辽东半岛南部早白垩世变质核杂岩时空分布及动力学特征[J].地质与资源,2020,29(5):411-418. |
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