冀东-辽西太古宙火成岩岩石组合和动力学意义

刘树文; 王伟; 白翔; 郭荣荣; 付敬浩; 郭博然; 胡方泱; 王茂江

doi:10.3799/dqkx.2018.003

Volume 43 Issue 1

Jan. 2018

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Liu Shuwen, Wang Wei, Bai Xiang, Guo Rongrong, Fu Jinghao, Guo Boran, Hu Fangyang, Wang Maojiang, 2018. Lithological Assemblages of Archean Meta-Igneous Rocks in Eastern Hebei-Western Liaoning Provinces of North China Craton, and Their Geodynamic Implications. Earth Science, 43(1): 44-56. doi: 10.3799/dqkx.2018.003

Citation:

Liu Shuwen, Wang Wei, Bai Xiang, Guo Rongrong, Fu Jinghao, Guo Boran, Hu Fangyang, Wang Maojiang, 2018. Lithological Assemblages of Archean Meta-Igneous Rocks in Eastern Hebei-Western Liaoning Provinces of North China Craton, and Their Geodynamic Implications. Earth Science, 43(1): 44-56. doi: 10.3799/dqkx.2018.003

Citation:

Liu Shuwen, Wang Wei, Bai Xiang, Guo Rongrong, Fu Jinghao, Guo Boran, Hu Fangyang, Wang Maojiang, 2018. Lithological Assemblages of Archean Meta-Igneous Rocks in Eastern Hebei-Western Liaoning Provinces of North China Craton, and Their Geodynamic Implications. Earth Science, 43(1): 44-56. doi: 10.3799/dqkx.2018.003

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Lithological Assemblages of Archean Meta-Igneous Rocks in Eastern Hebei-Western Liaoning Provinces of North China Craton, and Their Geodynamic Implications

doi: 10.3799/dqkx.2018.003

1.
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education; School of Earth and Space Sciences, Peking University, Beijing 100871, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
3.
Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100294, China
4.
Key Laboratory of Ministry of Education on Safe Mining of Deep Metal Mines. School of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China
5.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

Received Date: 2017-09-27
Publish Date: 2018-01-15

Abstract

Abstract

The eastern Hebei-western Liaoning provinces are the largest exposure regions of Archean basement rocks in the northern part of North China Craton. Comprehensive studies including detailed mapping of lithological assemblages reveal that the Archean basement rocks in the study regions can be subdivided into eight different assemblages, i.e., 2.64-2.60 Ga MORB-type metabasaltic rocks; 2.61-2.52 Ga metamorphosed tholeiitic to calc-alkaline volcanic rocks; 2.52-2.50 Ga calc-alkaline volcanic rocks with low metamorphic grade; 2.54-2.50 Ga tonalitic-trondhjemitic-granodioritic gneisses; 2.54-2.51 Ga dioritic-quartz dioritic-tonalitic-trondhjemitic-granodioritic gneisses; 2.54-2.51 Ga enderbites and charnockites; 2.57-2.52 Ga dioritic-quartz monzodioritic-granodioritic-monzogranitic gneisses; and 2.53-2.51 Ga weakly gneissic to massive monzogranitic to syenogranitic plutonic rocks. The above lithological assemblages show apparently banded spatial distribution patterns from Fuxin area of western Liaoning in the northeast to the Malanyu area of Zunhua in the southwest. Metamorphic studies indicate that high pressure granulites outcropped in the Qinglong-Shangying-Saheqiao areas record typical isothermal decompression (ITD)-type metamorphic P-T-t paths, which are associated with the thrusting structures from NNW-NW to SSE-SE. In contrast, isobaric cooling (IBC)-type metamorphic P-T-t paths are recorded by the high-temperature granulites from Santunying-Taipingzhai areas, which were accompanied by extensional diapiric structures in the Jinzhou-Xingcheng-Anziling-Jiehekou-Taipingzhai-Santunying regions. Accordingly, it is suggested that the Late Archean tectonothermal events in the eastern Hebei-western Liaoning provinces could have been generated under a typical Archean hot orogenic belt, evolving from subduction and back-arc extension to the final collision.

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Lithological Assemblages of Archean Meta-Igneous Rocks in Eastern Hebei-Western Liaoning Provinces of North China Craton, and Their Geodynamic Implications

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