Age marks in bottom sediments of the Pacific Ocean

Distribution of K-Ar age marks in Pacific bottom sediments is shown on the base of large analytical material. Dependence of K-Ar age marks on abundance of potassium-bearing authigenic diagenetic minerals (glauconite, phillipsite) widely spread in the studied part of the World Oceans.

Bibliographic Details
Main Authors: Krylov, AYa, Lisitzina, Nadezhda A, Mazina, T I, Silin, YuI, Tsovbun, Ya M
Format: Dataset
Language:English
Published: PANGAEA 1984
Subjects:
6-51A
6-53
6-59B
6-60
Archive of Ocean Data
ARCOD
Bering Sea
Central Basin
Pacific Ocean
Deep Sea Drilling Project
DM8
DM8-515
DM9
DM9-612
DM9-613
DM9-627
DM9-641
DM9-643
DM9-645
DM9-649
DM9-669
DM9-675
Dmitry Mendeleev
DRILL
Drilling/drill rig
DSDP
Eastern Basin
Equatorial Pacific
GC
Glomar Challenger
Gravity corer
KLMSTS-BS
KLMSTS-NNS
Leg6
Mariana Basin
MULT
Multiple investigations
Northeast Pacific
North Pacific
North Pacific/Philippine Sea/RIDGE
North Pacific/PLAIN
North Pacific/TRENCH
Northwest Pacific
Ob1
Ob1-78
OKEAN
Okean Grab
PC
Pacific
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.777543
https://doi.org/10.1594/PANGAEA.777543
Description
Summary:Distribution of K-Ar age marks in Pacific bottom sediments is shown on the base of large analytical material. Dependence of K-Ar age marks on abundance of potassium-bearing authigenic diagenetic minerals (glauconite, phillipsite) widely spread in the studied part of the World Oceans.

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