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地球与行星物理

ISSN  2096-3955

CN  10-1502/P

Citation: ChengWei Yang, ChengHu Wang, GuiYun Gao, Pu Wang, 2022: Cretaceous–Cenozoic regional stress field evolution from borehole imaging in the southern Jinzhou area, western Liaoning, North China Craton, Earth and Planetary Physics. http://doi.org/10.26464/epp2022001

doi: 10.26464/epp2022001

Cretaceous–Cenozoic regional stress field evolution from borehole imaging in the southern Jinzhou area, western Liaoning, North China Craton

1National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China;

2School of Civil Engineering, Tianjin University, Tianjin 300072, China

Fund Project: This study is supported by the National Natural Science Foundation of China (41574088). Helps from Mr. Hao Zhou, Xueyong Wei, Nian Chen and Hong Wang are appreciated.

The Mesozoic Yanshanian Movement affected the tectonic evolution of the North China Craton (NCC). It is proposed that Mesozoic cratonic destruction peaked ~125 Ma, possibly influenced by subduction of the western Pacific Plate beneath the Euro-Asian Plate in the Early Cretaceous. The southern Jinzhou area in the eastern block of the NCC preserves records for the tectonic events and related geological resources. Studies of the regional stress field evolution from the Cretaceous to Cenozoic can enhance our understanding of the tectonics and dynamics of the NCC. Borehole image logging technology was used to identify and collect attitudes of tensile fractures from 11 boreholes, which were subdivided into four groups according to dip directions, i.e., NNW-SSE, NWW-SEE, W-E and NE-SW. Their development was mainly controlled by the regional tectonic stress field while temperature, lithology, and depth contributed to some extent. The area was characterized by NNW-SSE- and NWW-SEE-oriented extension in 136-125 Ma in the Early Cretaceous. Subsequently, it has successively undergone W-E- and NE-SW-oriented extension in 125-101 Ma and after 101 Ma. This counterclockwise trend has persisted to the present, probably related to oblique subduction of the Pacific Plate and is characterized by ongoing nearly N-S-oriented extension and NEE-SWW-oriented compression.

Key words: stress field, tensile fracture, borehole, southern Jinzhou, North China Craton

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Cretaceous–Cenozoic regional stress field evolution from borehole imaging in the southern Jinzhou area, western Liaoning, North China Craton

ChengWei Yang, ChengHu Wang, GuiYun Gao, Pu Wang