Clastic sediment records of the Philippine and Japan Seas

Fuente: PANGAEA
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Autore principale: Nechaev, Victor P
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1991
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author Nechaev, Victor P
author_facet Nechaev, Victor P
collection Datos científicos de ciencias marinas y ambientales
contents Mineralogical analyses of the heavy coarse silt fraction, including microprobe identifications of certain clastic minerals, and bulk chemical analyses of 186 sediment samples from DSDP sites 291, 299, 301, 436, 447, 449, 450, 453, 459 and 460 are compared with similar data for Quaternary sediments on a profile across the Pacific from Central America to the Far East. As a result, new details of the history of the Philippine and Japan Seas suggest that the active marginal complex has a variety of "states" (stages). These states differ in terms of (1) the number of associated "echelons" (i.e. parts of the complex), each consisting of a subduction zone, island arc and back-arc basin situated one behind the other, and (2) their orientations. Changes in state are caused by blocking, i.e. hindering, the subduction. Continental as well as oceanic lithosphere is involved in the system. The "island arc" lithosphere, which is more simatic than continental lithosphere and more sialic than oceanic lithosphere, is a final product of the development of the marginal complex irrespective of whether the parent was continental or oceanic lithosphere.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_760257
institution PANGAEA
language en
publishDate 1991
publisher PANGAEA
record_format pangaea
spellingShingle Clastic sediment records of the Philippine and Japan Seas
Nechaev, Victor P
31-291; 31-291A; 31-299; 31-301; 56-436; 59-447A; 59-449; 59-450; 60-453; 60-459B; 60-460; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg31; Leg56; Leg59; Leg60; North Pacific/BASIN; North Pacific/Japan Sea; North Pacific/Japan Sea/CONT RISE; North Pacific/Philippine Sea/BASIN; North Pacific/Philippine Sea/TRENCH; North Pacific/RIDGE; North Pacific/SEDIMENT POND
Mineralogical analyses of the heavy coarse silt fraction, including microprobe identifications of certain clastic minerals, and bulk chemical analyses of 186 sediment samples from DSDP sites 291, 299, 301, 436, 447, 449, 450, 453, 459 and 460 are compared with similar data for Quaternary sediments on a profile across the Pacific from Central America to the Far East. As a result, new details of the history of the Philippine and Japan Seas suggest that the active marginal complex has a variety of "states" (stages). These states differ in terms of (1) the number of associated "echelons" (i.e. parts of the complex), each consisting of a subduction zone, island arc and back-arc basin situated one behind the other, and (2) their orientations. Changes in state are caused by blocking, i.e. hindering, the subduction. Continental as well as oceanic lithosphere is involved in the system. The "island arc" lithosphere, which is more simatic than continental lithosphere and more sialic than oceanic lithosphere, is a final product of the development of the marginal complex irrespective of whether the parent was continental or oceanic lithosphere.
title Clastic sediment records of the Philippine and Japan Seas
topic 31-291; 31-291A; 31-299; 31-301; 56-436; 59-447A; 59-449; 59-450; 60-453; 60-459B; 60-460; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg31; Leg56; Leg59; Leg60; North Pacific/BASIN; North Pacific/Japan Sea; North Pacific/Japan Sea/CONT RISE; North Pacific/Philippine Sea/BASIN; North Pacific/Philippine Sea/TRENCH; North Pacific/RIDGE; North Pacific/SEDIMENT POND
url https://doi.org/10.1594/PANGAEA.760257