The role and significance of structural deformation in metamorphic rock mapping:A case study of the Liaohe Group mapping in central segment of Jiao-Liao-Ji orogenic belt

TIAN Zhonghua; LIU Fulai; XU Wang; JI Lei; LIU Lishuang; DONG Yongsheng

2017 Vol. 36, No. 11

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TIAN Zhonghua, LIU Fulai, XU Wang, JI Lei, LIU Lishuang, DONG Yongsheng. The role and significance of structural deformation in metamorphic rock mapping:A case study of the Liaohe Group mapping in central segment of Jiao-Liao-Ji orogenic belt[J]. Geological Bulletin of China, 2017, 36(11): 1942-1952.

Citation:

TIAN Zhonghua, LIU Fulai, XU Wang, JI Lei, LIU Lishuang, DONG Yongsheng. The role and significance of structural deformation in metamorphic rock mapping:A case study of the Liaohe Group mapping in central segment of Jiao-Liao-Ji orogenic belt[J]. Geological Bulletin of China, 2017, 36(11): 1942-1952.

The role and significance of structural deformation in metamorphic rock mapping:A case study of the Liaohe Group mapping in central segment of Jiao-Liao-Ji orogenic belt

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
College of Earth Sciences, Jilin university, Changchun 130061, Jilin, China

Received Date: 09 March 2017

Revised Date: 20 May 2017

Publish Date: 25 November 2017

Abstract

Abstract

Based on the mapping of the Liaohe Group in the central segment of Jiao-Liao-Ji structural belt in the past several years, this paper mainly presents the implications of structural deciphering work applied to the metamorphic area geological mapping, which include the following five aspects:①As the significant geological boundary between the groups cannot be easily recognized, the authors emphasize the function of structural deciphering work when it is used to trace the hidden boundary; ②Different rock units or formations are often mixed with each other due to later deformation, and structural deciphering therefore should be used in this situation to distinguish different rock units (strata); ③Structural deciphering work must be carried out to trace all the different structural styles and deformation stages; ④Evaluation of the thickness of strata in the metamorphic area should be considered through structural deciphering work in the first time; ⑤The combination of deformation and metamorphism is very important in metamorphic mapping area. In all, structural deciphering is a useful tool to figure out the true geological fact in a metamorphic mapping area.
- specific geological mapping /
- mapping method /
- structural deciphering /
- metamorphic region /
- Liaohe Group

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References

[1]	Barnes J W, Lisle R J. Basic Geological mapping[M]. John Wiley & Sons, 2004. Google Scholar
[2]	Norman F. The Field Description of Metamorphic rocks[M]. John Wiley & Sons, 1984. Google Scholar
[3]	Tucker M E. Sedimentary Rocks in the Field[M]. John Wiley & Sons, 2011. Google Scholar
[4]	Jerram D, Petford N. The Field Description of Igneous rocks[M].John Wiley & Sons, 2011. Google Scholar
[5]	McClay K R. The Mapping of Geological Structures[M]. John Wiley & Sons, 1991. Google Scholar
[6]	Passchier C W, Myers J S, Kröner A. Field Geology of High-Grade Gneiss Terrains[M]. Springer-Verlag Berlin Heidelberg, 1990. Google Scholar
[7]	房立民, 杨振升, 李勤, 等.变质岩区1:5万区域地质填图方法指南(地质矿产部直属单位管理局)[M].武汉:中国地质大学出版社, 1991. Google Scholar
[8]	Spalla M I, Di Paola S, Gosso G, et al. Mapping tectono-metamorphic histories in the Lake Como basement (Southern Alps, Italy)[J]. Memorie di Scienze, Geologiche, 2002, 54:101-134. Google Scholar
[9]	Brogi A. Foliation relationships and structural facing vs. vergence determinations in refolded low-grade metamorphic rocks:an example from the Tuscan Metamorphic'Basement'(Northern Apennines, Italy)[J]. Journal of Structural Geology, 2006, 28:115-128. doi: 10.1016/j.jsg.2005.07.009 CrossRef Google Scholar
[10]	Philippon M, Le Carlier de Veslud C, Gueydan F, et al. 3D geometrical modelling of post-foliation deformations in metamorphic terrains (Syros, Cyclades, Greece)[J]. Journal of Structural Geology, 2015, 78:134-148. doi: 10.1016/j.jsg.2015.07.002 CrossRef Google Scholar
[11]	Vollgger S A, Cruden A R. Mapping folds and fractures in basement and cover rocks using UAV photogrammetry, Cape Liptrap and Cape Paterson, Victoria, Australia[J]. Journal of Structural Geology, 2016, 85, 168-187. doi: 10.1016/j.jsg.2016.02.012 CrossRef Google Scholar
[12]	胡国巍.早元古代辽河群的基本构造特征[J].中国地质科学院天津地质矿产研究所文集, 1992, 26/27:179-188. Google Scholar
[13]	白瑾.华北陆台北缘前寒武纪地质及铅锌成矿作用[M].北京:地质出版社, 1993. Google Scholar
[14]	李三忠, 杨振升, 刘永江, 等.胶辽吉地区古元古代早期花岗岩的侵位模式及其与隆滑构造的关系[J].岩石学报, 1997, 64-77. Google Scholar
[15]	Zhao G C, Cawood P A, Li S Z, et al. Amalgamation of the North China Craton:Key issues and discussion[J]. Precambrian Research, 2012, 222/223:55-76. doi: 10.1016/j.precamres.2012.09.016 CrossRef Google Scholar
[16]	刘福来, 刘平华, 王舫, 等.胶-辽-吉古元古代造山/活动带巨量变沉积岩系的研究进展[J].岩石学报, 2015, 31(10):2816-2846. Google Scholar
[17]	Li S Z, Zhao G C, Sun M, et al. Deformation history of the Paleoproterozoic Liaohe assemblage in the eastern block of the North China Craton[J]. Journal of Asian Earth Sciences, 2005, 24:659-674. doi: 10.1016/j.jseaes.2003.11.008 CrossRef Google Scholar
[18]	辽宁省地质矿产局(LBG).辽宁省区域地质志[M].北京:地质出版社, 1989:33-55. Google Scholar
[19]	辽宁省地质矿产局(LBG).辽宁省1:20万辽阳市幅地质报告[M].北京:地质出版社, 1975. Google Scholar
[20]	单文琅, 傅昭仁.区域变质岩区填图的构造地层学准则[J].地球科学, 1987, 5:559-566. Google Scholar
[21]	王五力.试论构造地层学、非史密斯地层学和造山带地层学[J].地层学杂志, 2000, S1:352-358. Google Scholar
[22]	竺国强.构造地层学是变质岩地区地层研究的有效方法[J].中国地质, 1987, 10:19-20. Google Scholar
[23]	Zhao G C, Sun M, Wilde S A, et al. Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited[J]. Precambrian Research, 2005, 136:177-202. doi: 10.1016/j.precamres.2004.10.002 CrossRef Google Scholar
[24]	Tian Z H, Liu F L, Windley B F, et al. Polyphase structural deformation of low-to medium-grade metamorphic rocks of the Liaohe Group in the Jiao-Liao-Ji Orogenic Belt, North China Craton:correlations with tectonic evolution[J]. Precambrian Research, 2017, DOI:https://doi.org/10.1016/j.precamres.2017.08.017. Google Scholar
[25]	Lu, X P, Wu F Y, Guo, J H, et al. Zircon U-Pb geochronological constraints on the Paleoproterozoic crustal evolution of the Eastern block in the North China Craton[J]. Precambrian Research, 2006, 146:138-164. doi: 10.1016/j.precamres.2006.01.009 CrossRef Google Scholar
[26]	贺高品, 叶惠文.辽东-吉南地区早元古代两种类型变质作用及其构造意义[J].岩石学报, 1998, 14(2):152-162. Google Scholar
[27]	卢良兆, 徐学纯, 刘福来.中国北方早前寒武纪孔兹岩系[M].长春:长春出版社, 1996:195-234. Google Scholar