Late Cenozoic tectonic evolution of the southern segment of the Tan-Lu fault zone, Eastern China

2019 ◽  
Vol 182 ◽  
pp. 103932
Author(s):  
Ren Jiang ◽  
Kai Cao ◽  
Jianwei Zeng ◽  
Kai Liu ◽  
Changbo Li ◽  
...  
2002 ◽  
Vol 114 (9) ◽  
pp. 1159-1173 ◽  
Author(s):  
Stuart N. Thomson

Abstract Fission-track (FT) thermochronology has been applied to investigate the low-temperature cooling and denudation history of the Patagonian Andes along the southern part of the intra-arc transpressional Liquiñe-Ofqui fault zone between 42° and 46°S. The Liquiñe-Ofqui fault is shown to have been the focus of enhanced cooling and denudation initiated between ca. 16 and 10 Ma. Several fault blocks with different cooling histories are identified; these are separated by major oblique- or reverse-slip faults proposed to form the eastern part of a major (crustal-scale) dextral transpression zone. Local very fast rates of cooling and denudation between ca. 7 and 2 Ma were coeval with collision of the Chile Rise (an active mid-oceanic ridge) with the Peru-Chile Trench between ∼47° and 48°S. This location is close to the southern termination of the Liquiñe-Ofqui fault, implying that the collision of the ridge was a major force driving late Cenozoic transpression. The lack of significant cooling and denudation before ca. 16 Ma is indicative of pure strike-slip or transtensional movement along the Liquiñe-Ofqui fault before the collision of the ridge. Digital landscape analysis supports glacial and periglacial erosion as the main contributor to denudation since ca. 7 Ma, leading to restriction of topographic development. The combination of transpression-induced rock uplift and glacial erosion is shown to be very effective at causing localized denudation. Anomalously young FT ages along the Liquiñe-Ofqui fault are attributed to the existence of a late Cenozoic localized heat-flow anomaly along the fault.


2021 ◽  
Vol 14 (1) ◽  
Author(s):  
Yixin Dou ◽  
Guangzhou Mao ◽  
Lingqiang Meng ◽  
Xiaotong Liu ◽  
Pengrui An ◽  
...  

2019 ◽  
Vol 52 (10) ◽  
pp. 4133-4145
Author(s):  
Peng Li ◽  
Mei-feng Cai ◽  
Sheng-jun Miao ◽  
Qi-feng Guo

Energies ◽  
2018 ◽  
Vol 12 (1) ◽  
pp. 98 ◽  
Author(s):  
Shuai Jiang ◽  
Weifeng Wang ◽  
Aizhu Zhang ◽  
Weiwei Zhou

Covert fault zone is an important type of geological phenomenon that is closely related to hydrocarbon formation and distribution but has often been overlooked because it lacks obvious fault displacement and fault plane. To meet this challenge, a novel cognitive framework is proposed in this study, in which criteria for identifying the existence of covert fault zone are developed based on the regional tectonic backgrounds and geophysical data. The Riedel shear model is then utilized to analyze the genetic mechanism of the covert fault zone. The Mohr-Coulomb theory is also introduced to conduct a structural physical simulation to interpret the evolution process of the covert fault zone. Information about the genetic mechanism and evolution of the covert fault zone is finally combined to determine the oil-controlling mode. The study site is Qikou Sag in Eastern China. It is found that the covert fault zone in Qikou Sag meets four recognition criteria and is generated by the stress transferred from the strike-slip activity of the basement fault. Moreover, it can be concluded that the covert fault zone in Qikou Sag contains five evolution stages and controls the reservoir mainly via three aspects, that is, sedimentary sand, subtle traps and oil accumulation mode.


Lithos ◽  
2020 ◽  
Vol 366-367 ◽  
pp. 105561
Author(s):  
Yong-Wei Zhao ◽  
Haibo Zou ◽  
Ni Li ◽  
Wei Wei ◽  
Chao Yuan ◽  
...  

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