Apatite Fission Track Thermochronology and Its Tectonic Significance in Balikuntage of Eastern Tianshan

被引：0

作者：

Lu, Zongyue ^{[1
,2
,3
]}

Yu, Xinqi ^{[2
]}

Zhang, Feng ^{[4
]}

Hu, Jun ^{[2
]}

Wang, Zhaofan ^{[5
]}

Zeng, Yan ^{[6
]}

Sun, Kang ^{[1
,3
]}

Zhang, Wei ^{[1
,3
]}

机构：

[1] Center for Geophysical Survey, China Geological Survey, Hebei, Langfang

[2] School of Earth Sciences and Resources, China University of Geosciences, Beijing

[3] Technology Innovation Center for Earth Near Surface Detection, China Geological Survey, Hebei, Langfang

[4] Civil-Military Integration Center of China Geological Survey, Sichuan, Chengdu

[5] Haikou Marine Geological Investigation Center of China Geological Survey, Hainan, Haikou

[6] Wuhan Surveying-geotechnical Research Institute Co., Ltd. of MCC, Hubei, Wuhan

来源：

Geotectonica et Metallogenia | 2024年 / 48卷 / 04期

关键词：

apatite; Balikuntage; fission track; thermal history simulation;

D O I：

10.16539/j.ddgzyckx.2024.04.002

中图分类号：

学科分类号：

摘要：

In this paper, we present the tectonic evolution characteristics of Balikuntage in Eastern Tianshan on the basis of apatite fission track thermochronological analysis. The apatite fission track ages of (50±3) Ma to (58±5) Ma are obviously younger than the formation age of the rock mass, indicating that the samples underwent complete annealing. The average uplift rate of the four samples was 0.057 mm/a. The tectonic uplift in Balikuntage since Late Cretaceous can be divided into three stages. In the first stage (80–50 Ma), the mountain rose rapidly, responding to the accretion of Kohistan-Dras island arc in the Late Cretaceous and the initial collision between the Indian and Eurasian plates. In the second stage (50–20 Ma), the mountain was slowly uplifted. The third stage, 20 Ma to now, is the second rapid uplift period. The second and third stages were controlled by the far-range effects of the collision between the Indian and Eurasian plates. © 2024 Science Press. All rights reserved.

引用

页码：690 / 697

页数：7

共 35 条

[1] pp. 649-655
[2] 21, 1, pp. 249-260
[3] pp. 1011-1020
[4] 20, 1, pp. 81-92
[5] 3, pp. 319-331
[6] 巴里坤塔格晚古生代侵入岩岩石地球化学与Sr-Nd-Pb同位素特征, 西北地质, 48, 2, pp. 17-30, (2015)
[7] 西北地质, 48, 3, pp. 214-225
[8] 3, pp. 87-92
[9] 51, 4, pp. 463-469
[10] pp. 487-493

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