Variability of the bottom-simulating reflector (BSR) and its association with tectonic structures in the Chilean margin between Arauco Gulf (37°S) and Valdivia (40°S)-Reference-Cited by-同舟云学术

Variability of the bottom-simulating reflector (BSR) and its association with tectonic structures in the Chilean margin between Arauco Gulf (37°S) and Valdivia (40°S)

Published:2009-03 Issue:1 Volume:30 Page:1-19
ISSN:0025-3235
Container-title:Marine Geophysical Researches
language:en
Short-container-title:Mar Geophys Res

Author:

Rodrigo Cristián,González-Fernández Antonio,Vera Emilio

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Oceanography

Link

http://link.springer.com/content/pdf/10.1007/s11001-009-9064-2.pdf

Reference71 articles.

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2. Bangs NL, Cande SC (1997) Episodic development of a convergent margin inferred from structures and processes along the Southern Chile margin. Tectonics 16:489–503. doi: 10.1029/97TC00494

3. Bangs NB, Sawyer DS, Golovchenko X (1993) Free gas at the base of the gas hydrate zone in the vicinity of the Chile Triple Junction. Geology 21:905–908. doi: 10.1130/0091-7613(1993)021<0905:FGATBO>2.3.CO;2

4. Behrmann JH, Lewis SD, Musgrave RJ (1992) Proceedings of the Ocean Drilling Program. Initial Reports 141. College Station, TX, p 706

5. Brown KM, Bangs NL, Froelich PN, Kvenvolden KA (1996) The nature, distribution, and origin of gas hydrate in the Chile Triple Junction region. Earth Planet Sci Lett 139:471–483. doi: 10.1016/0012-821X(95)00243-6

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