Tectonic context of fluid venting at the toe of the eastern Nankai accretionary prism: Evidence for a shallow detachment fault
- 30 April 1992
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 109 (3-4) , 319-332
- https://doi.org/10.1016/0012-821x(92)90095-d
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Deep biological communities in the subduction zone of Japan from bottom photographs taken during “nautile” dives in the Kaiko projectPublished by Elsevier ,2002
- Mud volcano field seaward of the Barbados Accretionary Complex: A submersible surveyJournal of Geophysical Research, 1990
- Mud volcano field seaward of the Barbados Accretionary Complex: A deep‐towed side scan sonar surveyJournal of Geophysical Research, 1990
- Relationship between carbonate deposits and fluid venting: Oregon Accretionary PrismJournal of Geophysical Research, 1990
- Interrelationship of fluid venting and structural evolution: Alvin observations from the frontal accretionary prism, OregonJournal of Geophysical Research, 1990
- Detailed structure and possible fluid paths at the toe of the Barbados accretionary wedge (ODP Leg 110 area)Geology, 1990
- Tectonics and hydrogeology of accretionary prisms: role of the décollement zoneJournal of Structural Geology, 1989
- Tectonics and hydrogeology of the northern Barbados Ridge: Results from Ocean Drilling Program Leg 110GSA Bulletin, 1988
- Geophysical survey of a mud volcano seaward of the Barbados Ridge Accretionary ComplexJournal of Geophysical Research, 1988
- Nankai Trough and Zenisu Ridge: a deep-sea submersible surveyEarth and Planetary Science Letters, 1987