_version_ 1867170032343056384
author Deroo, Gerard
Herbin, Jean-Paul
author_facet Deroo, Gerard
Herbin, Jean-Paul
collection Datos científicos de ciencias marinas y ambientales
contents Pliocene-Pleistocene marls, muds, and hemipelagic clays with some beds of silt and sand were recovered on Leg 65 near the crest of the East Pacific Rise at the mouth of the Gulf of California. The organic matter in the sediments is mainly of marine origin for the upper Pleistocene sediments (0-0.61 m.y.), while the lower Pleistocene deposits (0.61- 1.80 m.y.) are characterized by continental organic matter except near the bottom of the sediment section in Hole 483A, where marine organic matter was found. The sediments belong to an early stage of geochemical evolution, except in Hole 482D, where hydrothermal effects are invoked to explain the maturity of the organic matter above the basement.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_818011
institution PANGAEA
language en
publishDate 1983
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Organic geochemistry of sediments recovered from DSDP Leg 65 Holes
Deroo, Gerard
Herbin, Jean-Paul
65-482; 65-482A; 65-482B; 65-482D; 65-483A; 65-483B; 65-483C; 65-484A; 65-485; 65-485A; Carbon, inorganic, total; Carbon, organic, total; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Elevation of event; Event label; Glomar Challenger; Hydrogen index, mass HC, per unit mass total organic carbon; Hydrogen index *; Index; Latitude of event; Leg65; Longitude of event; North Pacific/Gulf of California/CONT RISE; North Pacific/Gulf of California/DIAPIR; North Pacific/Gulf of California/SEDIMENT POND; Oxygen index, mass CO2, per unit mass total organic carbon; Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
Pliocene-Pleistocene marls, muds, and hemipelagic clays with some beds of silt and sand were recovered on Leg 65 near the crest of the East Pacific Rise at the mouth of the Gulf of California. The organic matter in the sediments is mainly of marine origin for the upper Pleistocene sediments (0-0.61 m.y.), while the lower Pleistocene deposits (0.61- 1.80 m.y.) are characterized by continental organic matter except near the bottom of the sediment section in Hole 483A, where marine organic matter was found. The sediments belong to an early stage of geochemical evolution, except in Hole 482D, where hydrothermal effects are invoked to explain the maturity of the organic matter above the basement.
title (Table 1) Organic geochemistry of sediments recovered from DSDP Leg 65 Holes
topic 65-482; 65-482A; 65-482B; 65-482D; 65-483A; 65-483B; 65-483C; 65-484A; 65-485; 65-485A; Carbon, inorganic, total; Carbon, organic, total; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Elevation of event; Event label; Glomar Challenger; Hydrogen index, mass HC, per unit mass total organic carbon; Hydrogen index *; Index; Latitude of event; Leg65; Longitude of event; North Pacific/Gulf of California/CONT RISE; North Pacific/Gulf of California/DIAPIR; North Pacific/Gulf of California/SEDIMENT POND; Oxygen index, mass CO2, per unit mass total organic carbon; Pyrolysis temperature maximum; Rock eval pyrolysis (Espitalié et al. 1977); Sample code/label
url https://doi.org/10.1594/PANGAEA.818011