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  4. CREATE III: 東亞地函動力及板塊互動研究─藏東與鄰近地區斷層帶剪切作用研究(1/3)
 
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CREATE III: 東亞地函動力及板塊互動研究─藏東與鄰近地區斷層帶剪切作用研究(1/3)

Date Issued
2004
Date
2004
Author(s)
羅清華  
DOI
922116M002006
URI
http://ntur.lib.ntu.edu.tw//handle/246246/11839
Abstract
The Song Ma belt, a suture zone located in between the South China and Indochina blocks, was offset by the Dien Bien Phu Fault (DBF) in northern Vietnam. Previous studies 2 suggested that the Dien Bien Phu Fault is one of the Tertiary shear zones, resulted from the Cenozoic extrusion tectonics due to the India-Eurasia collision. However, the timing of the movement along DBF is remained unknown due to lacking of age constraints. In order to reveal the movement age of DBF, schist samples from DBF and granites from the granite belt along the northern margin of the Indochina block, were dated by 40Ar-39Ar method in the present study. K-feldspar, hornblende, and biotite samples form granite plutons yield very different age ranges between the opposite sides of DBF. Hornblende separates from an undeformed granite, on the west side, exhibit plateau dates at around 277Ma. This age appears to be older than the early Triassic collision age (~245Ma) registered in the Song Ma suture zone (Lepvrier et al., 1997), indicating that arc magmatism may have actively occurred on the northern margin of the Indochina block, before the early Triassic collision. On the other hand, deformed granitic samples from the east side of DBF exhibit plateau ages of 218-230 Ma which are younger than the collision age, which are close to the age range previously reported for the Truong Son belt (a shear belt formed during or after the early Triassic Indochina-South China collision event). Surprisingly, biotites and muscovites extracted from the schists collected from DBF, also show similar 40Ar/39Ar ages ranging form 192Ma to 211Ma, which are close to the deformation age of the Truong Son belt. This indicates that the Dien Bien Phu Fault and the Truong Son Fault may have formed a conjugate fault system, activated by the early Triassic collision event during the Indosinian Orogeny. Whether the Dien Bien Phu Fault has once been reactivated by the Tertiary India-Eurasia collision, or not? This question is still waiting for answer.
Subjects
40Ar/39Ar
Dien Bien Phu Fault
Vietnam
Publisher
臺北市:國立臺灣大學地質科學系暨研究所
Type
report
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