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author:

Lyu, G. (Lyu, G..) [1] | Jiao, J. (Jiao, J..) [2] | Zhang, B. (Zhang, B..) [3] | Lyu, C. (Lyu, C..) [4] | Wang, Z. (Wang, Z..) [5] | Wang, H. (Wang, H..) [6] | Wang, C. (Wang, C..) [7] (Scholars:王翠芝)

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Scopus PKU CSCD

Abstract:

Based on the study of gold field structure in Jiaodong area, a new model is put forward which developed as "magma core complex uplift - detachment zone structure" links detachment zone structure and magmatic core complex, and metamorphic core complex structure was not developed in the Mesozoic area.In this study, after more than 10 years of tectonic deformation and alteration lithofacies mapping, magmatic structure mapping, paleomagnetic research and kinematic survey, combined with geophysical data analysis, it is found that the typical "Linglong magmatic core complex uplift and detachment zone structure" in Jiaodong area shows a long-round arch dome.The geological phenomena show: ①The dome core is composed of multi-stage and multi-structural granitic complexes; ②The granitic complex is trapped by faults, and these detachment zones and shovel type fractures with low and middle-angles are shear fractured.The broad fracture zones show superposition of ductile and brittle deformation and post-magmatic hydrothermal metasomatic alteration mineralization; ③The hanging wall rocks of the detachment fault are distributed around the magmatic core, and are composed of basement metamorphic rocks and Mesozoic sedimentary rocks, showing a state of detachment depression.The "magmatic core complex uplift-detachment zone structure" is a new model conforming to the East Asian intracontinental tectono-magmatic activation background.Through the study of magma core complex uplift - detachment zone structure, it is proposed that magmatic uplift and pull-apart basin belong to the same tectonic system, extruding tectonic-magmatic uplift and extensional detachment depressions are the products of stress field transformation process, and disintegrating shovel fault and brittle ductile superposition tectonic-rock belt are the targets of metallogenic prediction.Regional diagenetic and metallogenic laws are taken as the mark of direct observation and exploration, and regional geological and metallogenic laws are studied.Geological survey and metallogenic prediction have extensive popularization value and demonstration significance. © 2023 China Geological Survey. All rights reserved.

Keyword:

brittle-ductile superposition detachment-shovel fracture zone granitic crystalline structure Jiaodong area magmatic core complex magmatic core complex uplift-detachment zone structure

Community:

  • [ 1 ] [Lyu G.]Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China
  • [ 2 ] [Lyu G.]School of Earth Science and Resources, Chang'an University, Shaanxi, Xi'an, 710054, China
  • [ 3 ] [Lyu G.]China University of Geosciences(Beijing), Beijing, 100083, China
  • [ 4 ] [Jiao J.]School of Earth Science and Resources, Chang'an University, Shaanxi, Xi'an, 710054, China
  • [ 5 ] [Zhang B.]Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
  • [ 6 ] [Lyu C.]Development Research Center, China Geological Survey, Beijing, 100037, China
  • [ 7 ] [Wang Z.]Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China
  • [ 8 ] [Wang H.]Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China
  • [ 9 ] [Wang C.]School of Zijin Mining and Geology, Fuzhou University, Fujian, Fuzhou, 350108, China

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Source :

地质通报

ISSN: 1671-2552

CN: 11-4648/P

Year: 2023

Issue: 4

Volume: 42

Page: 489-509

Cited Count:

WoS CC Cited Count:

SCOPUS Cited Count:

ESI Highly Cited Papers on the List: 0 Unfold All

WanFang Cited Count:

Chinese Cited Count:

30 Days PV: 0

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