Cretaceous reactivation of the Deokpori Thrust, Taebaeksan Basin, South Korea, constrained by K-Ar dating of clayey fault gouge

被引:39
作者
Zwingmann, Horst [1 ,2 ,3 ]
Han, Raehee [4 ]
Ree, Jin-Han [5 ]
机构
[1] CSIRO Earth Sci & Resource Engn, Bentley, WA 6102, Australia
[2] Univ Western Australia, Sch Earth & Environm, Crawley, WA, Australia
[3] Curtin Univ, Dept Appl Geol, Perth, WA, Australia
[4] Korea Inst Geosci & Mineral Resources, Geol Environm Div, Taejon 305350, South Korea
[5] Korea Univ, Dept Earth & Environm Sci, Seoul 136701, South Korea
基金
新加坡国家研究基金会;
关键词
MESOZOIC TECTONICS; SHALLOW FAULTS; RB-SR; BELT; GEOCHRONOLOGY; COLLISION; NORTH; ROCKS; ASIA;
D O I
10.1029/2010TC002829
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Deokpori Thrust, juxtaposing the early Paleozoic Yeongwol-type Joseon Supergroup (Yeongwol Group) against the Duwibong-type Joseon Supergroup (Taebaek Group) in the Okcheon belt, is an important regional structure in the Phanerozoic tectonic evolution of Korea. Although the initiation of the thrust has recently been conjectured to occur during the Middle Jurassic Daebo tectonic event in a continental magmatic arc setting, its movement history has never been studied. We report timing of brittle reactivation of the thrust obtained from K-Ar dating of fault gouges in the core of the Deokpori Thrust zone. K-Ar illite age data of fault gouges suggest reactivation of the thrust at ca. 72 Ma after a contact metamorphism around 94 Ma. Our result is the first documentation of the reactivation of a major Jurassic 'Daebo' structure and the reactivation may represent a significant contractional tectonic event during the Late Cretaceous in the Korean Peninsula.
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页数:13
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