Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Marcus G. Langseth"'
Publikováno v:
Collected Reprint Series ISBN: 9781118782149
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1284269cdd0d4d730d97276d06d99b98
https://doi.org/10.1002/9781118782149.ch18
https://doi.org/10.1002/9781118782149.ch18
Autor:
Marcus G. Langseth
Publikováno v:
Terrestrial Heat Flow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b579880e5ed6f0d33e42877e8b3eab1
https://doi.org/10.1029/gm008p0058
https://doi.org/10.1029/gm008p0058
Autor:
Marcus G. Langseth, Eli A. Silver
Publikováno v:
Geophysical Research Letters. 23:891-894
Over 100 measurements of seafloor heat flow reveal that the accretionary complex adjacent to the Nicoya Peninsula is characterized by remarkably low heat flow; values over the accretionary prism average 28 mW/m², and values in the trench and the oce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03cfdd924f129d22f4ac20e6f002a47d
https://doi.org/10.1029/96gl00733
https://doi.org/10.1029/96gl00733
Publikováno v:
Journal of Geophysical Research: Solid Earth. 98:7921-7938
Recent measurements of in situ subseafloor pore pressure in sediment ponds on the flank of the Mid-Atlantic Ridge using a Pop Up Pore Pressure Instrument have provided important information regarding fluid exchange processes at the seafloor as well a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a6b07695a307c550f522c34e44d211e
https://doi.org/10.1029/93jb00153
https://doi.org/10.1029/93jb00153
Publikováno v:
Journal of Geophysical Research: Solid Earth. 98:4121-4142
The pattern of heat flow from the Barbados Ridge accretionary complex has been derived from marine surveys with heat flow probes, from measurements in drill holes, and from the depths of bottom-simulating seismic reflectors caused by gas hydrate. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32746dfaf79057fd51f1bd5bda16c561
https://doi.org/10.1029/92jb01853
https://doi.org/10.1029/92jb01853
Publikováno v:
Geophysical Research Letters. 19:517-520
A comprehensive survey of heat flow, sediment thickness and bathymetry in a large intermontane sediment pond on the western flank of the Mid-Atlantic Ridge (North Pond) shows that only 20 to 25% of the heat escaping from the lithosphere flows through
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2467a600e247cd8e59a4a588377f4224
https://doi.org/10.1029/92gl00079
https://doi.org/10.1029/92gl00079
Autor:
Marcus G. Langseth, J. Casey Moore
Publikováno v:
Journal of Geophysical Research. 95:8737
Accretionary prisms, which develop from materials scraped from the subducting oceanic lithosphere, form within one of the most dynamic structural environments on Earth and constitute critical elements of mountain belts. In the marine setting these la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::166ce5b5fcefa5b1672074119cb3a046
https://doi.org/10.1029/jb095ib06p08737
https://doi.org/10.1029/jb095ib06p08737
Publikováno v:
Journal of Geophysical Research. 95:8829
Three E-W transects of closely spaced heat flow measurements across the Barbados Accretionary Complex are reported. One transect, about 100 km in length at 14°20′N and a shorter 15-km line at 14°35′N show that heat flow decreases arcward roughl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::59db5d6a86043ccbc6c8e92344197b6b
https://doi.org/10.1029/jb095ib06p08829
https://doi.org/10.1029/jb095ib06p08829
Publikováno v:
Journal of Geophysical Research. 95:9343
Pore fluids are passively convecting through young oceanic sediments and crust around Deep Sea Drilling Project (DSDP) site 504 on the southern flank of the Costa Rica Rift, as inferred from a variety of geological, geochemical, and geothermal observ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5d7ba8cd9201ec5d99aab8dc7f215d01
https://doi.org/10.1029/jb095ib06p09343
https://doi.org/10.1029/jb095ib06p09343
Autor:
Marc F. Benedetti, Jean-Paul Foucher, Siegfried Lallemant, X. LePichon, Pierre Henry, Graham K. Westbrook, Michael A. Hobart, Marcus G. Langseth
Publikováno v:
Journal of Geophysical Research. 95:8859
Detailed patterns of near surface tectonics and heat flow were investigated at two locations at the toe of the Barbados Ridge accretionary prism. At the two locations, in the thickly sedimented southern portion of the prism near 12°20′N and in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc55ad7a8f16975cc089895a6b1b1f6e
https://doi.org/10.1029/jb095ib06p08859
https://doi.org/10.1029/jb095ib06p08859