Comparison of measured and BSR-derived heat flow values, Makran accretionary prism, Pakistan
- 1 February 2000
- journal article
- Published by Elsevier in Marine Geology
- Vol. 164 (1-2) , 37-51
- https://doi.org/10.1016/s0025-3227(99)00125-5
Abstract
No abstract availableFunding Information
- Bundesministerium für Bildung und Forschung (AZ BEO 03G0 124 A.)
This publication has 26 references indexed in Scilit:
- Sediment dewatering in the Makran accretionary prismPublished by Elsevier ,2002
- Sediment deformation and plate tectonics in the Gulf of OmanPublished by Elsevier ,2002
- Predicting the occurrence, distribution, and evolution of methane gas hydrate in porous marine sedimentsJournal of Geophysical Research, 1999
- Velocity‐porosity relationships for water‐saturated siliciclastic sedimentsJournal of Geophysical Research, 1998
- Internal deformation and compaction of the Makran accretionary wedgeTerra Nova, 1997
- Deep-ocean field test of methane hydrate formation from a remotely operated vehicleGeology, 1997
- Methane hydrate stability in seawaterGeophysical Research Letters, 1994
- Seismic velocities and inferred porosities in the accretionary wedge sediments at the Cascadia marginJournal of Geophysical Research, 1994
- Estimates of heat flow derived from gas hydratesGeology, 1982
- Heat flow and age of the Gulf of OmanEarth and Planetary Science Letters, 1981