Mineralogy and geochemistry of volcanic ash at Japan Trench from DSDP Legs 87 and 57

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Hauptverfasser: Fujioka, Kantaro, Cadet, Jean-Paul, Morin, Jean-Claude
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 1986
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author Fujioka, Kantaro
Cadet, Jean-Paul
Morin, Jean-Claude
author_facet Fujioka, Kantaro
Cadet, Jean-Paul
Morin, Jean-Claude
collection Datos científicos de ciencias marinas y ambientales
contents Volcanogenic sediments were obtained from Site 584, located on the midslope of the Japan Trench. Occurrences of volcanic ash in the diatomaceous mudstones increase within sediments dated 6-3 Ma. The frequency pattern and the sediment accumulation rate obtained at Site 584 are similar to those of Site 440 and to those of Sites 438 and 439, located on the upper slope basin. Explosive volcanism increased during the Pliocene and late Miocene in relation to the intrusion of Tertiary granites and uplift of the Tohoku Arc (northeastern Japan Arc). Hygromagmaphile element concentration shows that the glass does not belong to a unique series, and a comparison with Nankai Trough data distinguishes at least two different evolutionary lines.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_801675
institution PANGAEA
language en
publishDate 1986
publisher PANGAEA
record_format pangaea
spellingShingle Mineralogy and geochemistry of volcanic ash at Japan Trench from DSDP Legs 87 and 57
Fujioka, Kantaro
Cadet, Jean-Paul
Morin, Jean-Claude
57-438A; 57-438B; 57-439; 57-440B; 87-582B; 87-583A; 87-584; 87-584A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg57; Leg87; North Pacific/BASIN; North Pacific/TRENCH; North Pacific Ocean
Volcanogenic sediments were obtained from Site 584, located on the midslope of the Japan Trench. Occurrences of volcanic ash in the diatomaceous mudstones increase within sediments dated 6-3 Ma. The frequency pattern and the sediment accumulation rate obtained at Site 584 are similar to those of Site 440 and to those of Sites 438 and 439, located on the upper slope basin. Explosive volcanism increased during the Pliocene and late Miocene in relation to the intrusion of Tertiary granites and uplift of the Tohoku Arc (northeastern Japan Arc). Hygromagmaphile element concentration shows that the glass does not belong to a unique series, and a comparison with Nankai Trough data distinguishes at least two different evolutionary lines.
title Mineralogy and geochemistry of volcanic ash at Japan Trench from DSDP Legs 87 and 57
topic 57-438A; 57-438B; 57-439; 57-440B; 87-582B; 87-583A; 87-584; 87-584A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg57; Leg87; North Pacific/BASIN; North Pacific/TRENCH; North Pacific Ocean
url https://doi.org/10.1594/PANGAEA.801675