鲁西新太古代洋板块地质及板块构造活动遗迹

陆松年; 相振群

doi:10.3799/dqkx.2020.047

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2279-2292

Lu Songnian, Xiang Zhenqun, 2020. Tracing Archives of Ocean Plate Geology and Tracking Plate Tectonics from the Neoarchean Granite-Greenstone Belt of the Western Shandong Province. Earth Science, 45(7): 2279-2292. doi: 10.3799/dqkx.2020.047

Citation:

Lu Songnian, Xiang Zhenqun, 2020. Tracing Archives of Ocean Plate Geology and Tracking Plate Tectonics from the Neoarchean Granite-Greenstone Belt of the Western Shandong Province. Earth Science, 45(7): 2279-2292. doi: 10.3799/dqkx.2020.047

Citation:

Lu Songnian, Xiang Zhenqun, 2020. Tracing Archives of Ocean Plate Geology and Tracking Plate Tectonics from the Neoarchean Granite-Greenstone Belt of the Western Shandong Province. Earth Science, 45(7): 2279-2292. doi: 10.3799/dqkx.2020.047

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Tracing Archives of Ocean Plate Geology and Tracking Plate Tectonics from the Neoarchean Granite-Greenstone Belt of the Western Shandong Province

doi: 10.3799/dqkx.2020.047

Lu Songnian^{1, 2
,
,},
Xiang Zhenqun^{1, 2}

1.
Tianjin Centre, China Geological Survey, Tianjin 300170, China
2.
Precambrain Geological Research Centre, China Geological Survey, Tianjin 300170, China

Received Date: 2020-03-11
Publish Date: 2020-07-15

Abstract

Abstract

The Luxi district which is located in West Shandong Province is one of the most representative granite-greenstone belts in the Neoarchean of China. Our pioneers have already accumulated rich sources related to tectonic lithostratigraphy, isotopic geochronology, geochemistry, mineralization, and etc. Some geologists also explores progressively the geodynamic features in this era. From the perspective of ocean plate geology, this article examines the previous data of regional geological investigation and research obtained by the predecessors, and shows that the mafic volcanic rocks of the Taishan Complex are composed of two rock associations, komatite-tholeiite and tholeiite-calc alkaline basalt-andesite, respectively. It reflects the evolution process from komatite related to mantle plume in the early stage to calc alkaline basalt-andesite related to arc in the late stage. From island arc type tonalite formed in the early stage of Neoarchean to differentiated trondhjemite formed in the middle stage of Neoarchean, it reflects the characteristics of granite evolution during subduction. The late Neoarchean Siliceous High Mg Basalt is the product of the active continental margin magma arc. The discovery of Ruby in the Taishan Complex further indicates that the setting of its formation is related to the subduction of Neoarchean plates. All these provide geological evidence for the existence of new Archean oceanic plate in Luxi District.
- western Shandong Province,
- Neoarchean,
- ocean plate geology,
- plate tectonics,
- tectonics

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References(78)

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