Theory and method of mapping the lower crust

ZHANG Qi; ZHAI Mingguo; WEI Chunjing; JIAO Shoutao; ZHOU Ligang; HUANG Guangyu; CHEN Wanfeng; TANG Jun; LIU Rui; YUAN Jie; WANG Zhen; WANG Yue; YUAN Fanglin

doi:10.12097/gbc.2023.01.030

2024 Vol. 43, No. 10

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ZHANG Qi, ZHAI Mingguo, WEI Chunjing, JIAO Shoutao, ZHOU Ligang, HUANG Guangyu, CHEN Wanfeng, TANG Jun, LIU Rui, YUAN Jie, WANG Zhen, WANG Yue, YUAN Fanglin. 2024. Theory and method of mapping the lower crust. Geological Bulletin of China, 43(10): 1673-1688. doi: 10.12097/gbc.2023.01.030

Citation:

ZHANG Qi, ZHAI Mingguo, WEI Chunjing, JIAO Shoutao, ZHOU Ligang, HUANG Guangyu, CHEN Wanfeng, TANG Jun, LIU Rui, YUAN Jie, WANG Zhen, WANG Yue, YUAN Fanglin. 2024. Theory and method of mapping the lower crust. Geological Bulletin of China, 43(10): 1673-1688. doi: 10.12097/gbc.2023.01.030

Theory and method of mapping the lower crust

1.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2.
State Key Laboratory of Lithospheric Evolution, Beijing 100029, China
3.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
4.
Natural Resources Comprehensive Survey Command Center, China Geological Survey, Beijing 100055, China
5.
Technology Innovation Center of Geological Information, MNR, Beijing 100055, China
6.
Key Laboratory of Mineral Resources in Western China (Gansu Province), School of Earth Sciences, Lanzhou University, Lanzhou 730000, Gansu, China
7.
School of Earth Sciences, Yangtze University, Wuhan 430100, China
8.
School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255000, Shandong, China
9.
School of Resources and Environment, Xingtai University, Xingtai 054001, Hebei, China
10.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
11.
School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China

Received Date: 29 January 2023

Revised Date: 28 November 2023

Publish Date: 15 October 2024

Abstract

Abstract

The condition of the lower crust in a region at a certain time is a question that has not been considered by academia, for the reason that there is no means. Our recent research on the origin of granite shows that granite is derived from partial melting of lower crust metamorphic rocks, and the granite is in equilibrium with the melt residual phase. Therefore, we can invert the characteristics of metamorphic rocks in the lower crust based on the characteristics of granite at the surface. On the other hand, the progress in the research of metamorphic rock indicate that it is possible to construct apparent profiles of metamorphic rocks of different compositions according to different temperature and pressure conditions, and to infer the properties of the melts formed during partial melting. The combination of these two aspects forms the theoretical basis for the mapping of the lower crustal, based on which to understand the conditions at the bottom of the lower crust, and thus the mapping method of the lower crust is derived. This paper discusses the method of mapping the lower crust, discusses the content of the lower crustal geological map that may be expressed in the current situation, focuses on the lower crustal information can be given by granite, and puts forward the principles for dealing with controversial issues. It also discusses how to map the lower crust in the absence of granite outcropping, and the information of the lower crust that may be provided by sedimentation, stratigraphy, paleontology, minerals, and structure are discussed, and the vitrinite reflectance method is recommended. In addition, the significance and limitations of lower crustal mapping are also discussed. At last, we discussed the function and significance of lower crust mapping by taking the geological map of the lower crust in the Early Cretaceous of Shanxi Province as an example.
- geological map of lower crust /
- mapping methods /
- granite /
- vitrinite reflectance

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References

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