Geological structure of the offshore Sumatra forearc region estimated from high-resolution MCS reflection survey
Autor: | Kohsaku Arai, Riza Rahardiawan, Ayanori Misawa, K. Hirata, Hiroshi Sarukawa, Yasuyuki Nakamura, Hisatoshi Baba, Toshiya Fujiwara, Juichiro Ashi, Haryadi Permana, Hidekazu Tokuyama, Masataka Kinoshita, Keita Adachi, Katsura Kameo, Udrekh, Yusuf S. Djajadihardja, Leonard Seeber |
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Rok vydání: | 2014 |
Předmět: |
geography
geography.geographical_feature_category Deformation (meteorology) Fault (geology) Geological structure Geophysics Space and Planetary Science Geochemistry and Petrology Trench Earth and Planetary Sciences (miscellaneous) Reflection (physics) Submarine pipeline Vergence (geology) Forearc Seismology Geology |
Zdroj: | Earth and Planetary Science Letters. 386:41-51 |
ISSN: | 0012-821X |
DOI: | 10.1016/j.epsl.2013.10.031 |
Popis: | To investigate detailed fault distributions and shallow geological structure offshore northwestern Sumatra, we obtained high-resolution Multi-Channel Seismic (MCS) reflection data around the Sunda Trench, trench slope, and forearc high regions offshore northwestern Sumatra. In general, trench-parallel anticlinal ridges are distributed from trench slope region to forearc high region. Two kinds of different vergence systems are characterized in the Sumatra forearc region; landward vergence is dominant in the lower trench slope region, and seaward vergence is dominant in the forearc high region. Moreover, piggyback or slope basins are recognized between anticlinal ridges. Deformation in the uppermost part of these basins, that is referred to ‘recent’ deformation in this paper, can be identified not only along major thrusts but also between major thrusts and the lower trench slope, suggesting these are related to recently active faulting. Several but the largest number of such deformation are distributed along a major thrust located in the middle of the forearc high region, whereas few are done along other major thrusts. |
Databáze: | OpenAIRE |
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