洋板块地质与川藏铁路工程地质关键区带

潘桂棠; 任飞; 尹福光; 王立全; 王保弟; 王冬兵; 安显银; 唐渊; 刘函; 王启宇; 庞维华; 徐波

doi:10.3799/dqkx.2020.070

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2293-2304

Pan Guitang, Ren Fei, Yin Fuguang, Wang Liquan, Wang Baodi, Wang Dongbing, An Xianyin, Tang Yuan, Liu Han, Wang Qiyu, Pang Weihua, Xu Bo, 2020. Key Zones of Oceanic Plate Geology and Sichuan-Tibet Railway Project. Earth Science, 45(7): 2293-2304. doi: 10.3799/dqkx.2020.070

Citation:

Pan Guitang, Ren Fei, Yin Fuguang, Wang Liquan, Wang Baodi, Wang Dongbing, An Xianyin, Tang Yuan, Liu Han, Wang Qiyu, Pang Weihua, Xu Bo, 2020. Key Zones of Oceanic Plate Geology and Sichuan-Tibet Railway Project. Earth Science, 45(7): 2293-2304. doi: 10.3799/dqkx.2020.070

Citation:

Pan Guitang, Ren Fei, Yin Fuguang, Wang Liquan, Wang Baodi, Wang Dongbing, An Xianyin, Tang Yuan, Liu Han, Wang Qiyu, Pang Weihua, Xu Bo, 2020. Key Zones of Oceanic Plate Geology and Sichuan-Tibet Railway Project. Earth Science, 45(7): 2293-2304. doi: 10.3799/dqkx.2020.070

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Key Zones of Oceanic Plate Geology and Sichuan-Tibet Railway Project

doi: 10.3799/dqkx.2020.070

1.
Chengdu Center, China Geological Survey, Chengdu 610081, China
2.
College of Geosciences, Chengdu University of Technology, Chengdu 610000, China

Received Date: 2020-04-08
Publish Date: 2020-07-15

Abstract

Abstract

The complex geological structure background of engineering geological difference in different zones of Sichuan-Tibet railway corridor is deconstructed,described the core idea and scientific significance of ocean plate geology.It is pointed out that there are seven oceanic subduction (Ophiolitic Melange belt) which accretion complex belts running through the Ya'an-Linzhi section of Sichuan-Tibet railway. With the strong uplift of the Qinghai-Tibet Plateau since Miocene,all of them are transformed into neotectonic active zone,active seismic zone,high geothermal active zone and geological disaster frequent zone. It is the key zone for Sichuan-Tibet railway. It is the key point of understanding that what is different geological background structure-rock combinations,different degrees of metamorphism,ordered or disordered structure of different deformation patterns,and restrict the behaviors of different rocks,soils and special unfavorable geological bodies; It is the key to complete the Sichuan-Tibet railway construction with high quality and high standard.
- ocean plate geology,
- subduction accretion complex,
- engineering geology,
- key engineering zone

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References(80)

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