Thermochronology of the Meso–Cenozoic uplift and tectonic growth of the Longmenshan Thrust Belt

JIN Wenzheng; WANG Shanmin; BAI Wankui; YE Zhixu

doi:10.12029/gc20220306001

2025 Vol. 52, No. 4

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JIN Wenzheng, WANG Shanmin, BAI Wankui, YE Zhixu. 2025. Thermochronology of the Meso–Cenozoic uplift and tectonic growth of the Longmenshan Thrust Belt[J]. Geology in China, 52(4): 1528-1542. doi: 10.12029/gc20220306001

Citation:

JIN Wenzheng, WANG Shanmin, BAI Wankui, YE Zhixu. 2025. Thermochronology of the Meso–Cenozoic uplift and tectonic growth of the Longmenshan Thrust Belt[J]. Geology in China, 52(4): 1528-1542. doi: 10.12029/gc20220306001

Thermochronology of the Meso–Cenozoic uplift and tectonic growth of the Longmenshan Thrust Belt

1.
School of Energy Resources, China University of Geosciences, Beijing 100083, China
2.
State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum (Beijing), Beijing 102249, China
3.
Geothermal Energy Science and Technology (Dali) Institute, Dali 671006, Yunnan, China
4.
Geophysical Research Institute of Sinopec Shengli Oilfield Branch, Dongying 257000, Shandong, China
5.
Jidong Oilfield Branch Company, PetroChina, Tangshan 063200, Hebei, China

Fund Project: Supported by National Natural Science Foundation of China “Study on the Mechanism of Structural Segmental Deformation in Longmenshan Thrust Belt” (No.41002072), Yunnan Province Science and Technology Plan “Research on Key Technologies for the Development and Utilization of Medium to Deep Geothermal Energy in Yunnan Province” (No. 202302AF080001), Open Fund of the State Key Laboratory of Oil and Gas Resources and Exploration “Thermochronological study on tectonic uplift of Bikou block since Mesozoic in northern Sichuan”(No.PRP/open-1307).

More Information

Author Bio: JIN Wenzheng, male, born in 1978, doctor, lecturer, mainly engaged in research of petroleum geology and basin analysis; E-mail: jwz@cugb.edu.cn

Received Date: 06 March 2022

Revised Date: 19 February 2023

Publish Date: 25 July 2025

Abstract

Abstract

This paper is the result of geological survey engineering.
Objective
This study focuses on the relationship between the vertical tectonic uplift and the lateral tectonic expansion that occurred during the Meso-Cenozoic in the Longmenshan thrust belt. To examine this relationship, low-temperature thermal chronology testing and analysis were conducted.
Methods
The characteristics of tectonic evolution were examined by determining and analyzing apatite and zircon fission track ages.
Results
The lengths of apatite fission tracks are within the range of (11.4 ± 2.6)–(12.2 ± 2.2) μm. This range effectively reflects the local tectonic uplift history. The thermal history simulation results show that the apatite samples experienced three critical stages: a rapid tectonic uplift, a stable tectonic stage, and a rapid tectonic uplift. The uplifting events occurred earlier in the northern area than in the southern area. The cooling rate of each rock sample was in the range of 1.211–6.053 °C/Ma. From the southeast to the northwest, the tectonic uplift rate increased gradually, while the time of uplifting was gradually delayed.
Conclusions
The Longmenshan thrust belt has undergone tectonic deformation characterized by piggyback propagation from northwest to southeast since the Meso−Cenozoic (150 Ma). This deformation continued from the Late Cretaceous to the Eocene (70–50 Ma) and persisted into the Oligocene (approximately 20 Ma). The central and western regions of the Longmenshan thrust belt are characterized by multi-stage tectonic uplift and superposition.
- tectonic uplift /
- tectonic extension /
- fission track /
- thermochronology /
- Meso−Cenozoic /
- geological survey engineering /
- Longmenshan

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References

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