欧亚北极区东部区域地质与构造演化

李学杰; 姚永坚; 杨楚鹏; 李波; 李涛

doi:10.3799/dqkx.2017.024

Volume 42 Issue 3

Mar. 2017

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Article Navigation > Earth Science > 2017 > 42(3): 315-324

Li Xuejie, Yao Yongjian, Yang Chupeng, Li Bo, Li Tao, 2017. Regional Geological Features and Tectonic Evolution in the Eastern Euroasian Arctic. Earth Science, 42(3): 315-324. doi: 10.3799/dqkx.2017.024

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Li Xuejie, Yao Yongjian, Yang Chupeng, Li Bo, Li Tao, 2017. Regional Geological Features and Tectonic Evolution in the Eastern Euroasian Arctic. Earth Science, 42(3): 315-324. doi: 10.3799/dqkx.2017.024

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Regional Geological Features and Tectonic Evolution in the Eastern Euroasian Arctic

doi: 10.3799/dqkx.2017.024

Guangzhou Marine Geological Survey, Key Laboratory of Marine Mineral Resouces, MLR, Guangzhou 510760, China

Received Date: 2016-09-30
Publish Date: 2017-03-15

Abstract

Abstract

Resources in eastern Arctic are quite abundant, however, a number of problems exist due to complicated regional geological structure and low degree of exploration. In this paper, the structure diagram of the study area is compiled, and the regional geological structure and its evolution are presented on the basis of a large collection of regional geological documents. The main tectonic units in the area include Verkhoyansk-Kolyma orogen, microplate of Arctic Alaska-Chukotka, Kolyma-Omolon superterrane, and South Anyui suture. As the open of Amerasia basin in Early Jurassic to Early Cretaceous, the microplate of Arctic Alaska-Chukotka rifted from the north margin of Canada. With the close of the Anui-Anvil (Angayucham) ocean, Alaska-Chukotka microplate collided with Kolyma-Omolon superterrane, resulting in the formation of South Anyui suture. Moreover, Verkhoyansk-Kolyma orogen resulted from collision between Verkhoyansk margin of Siberia continent and Kolyma-Omolon superterrane.
- regional geology,
- Euroasian Arctic,
- Verkhoyansk-Kolyma orogen,
- Novosibirsk-Chukchi-Brookian orogeny,
- tectonics,

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References(43)

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