Peculiarities of Clay Mineral Formation in Pleistocene Sediments Under Specific Tectonomagmatic and Hydrothermal Conditions of the Central Hill (Escanaba Trough, Gorda Ridge, Pacific Ocean): Communication 1. Hole ODP 1038B-Reference-Cited by-同舟云学术

Peculiarities of Clay Mineral Formation in Pleistocene Sediments Under Specific Tectonomagmatic and Hydrothermal Conditions of the Central Hill (Escanaba Trough, Gorda Ridge, Pacific Ocean): Communication 1. Hole ODP 1038B

Published:2024-09-02 Issue:5 Volume:59 Page:538-552
ISSN:0024-4902
Container-title:Lithology and Mineral Resources
language:en
Short-container-title:Lithol Miner Resour

Author:

Kurnosov V. B.,Sakharov B. A.,Konovalov Yu. I.,Savichev A. T.,Morozov I. A.,Korshunov D. M.

Publisher

Pleiades Publishing Ltd

Link

https://link.springer.com/content/pdf/10.1134/S0024490224700652.pdf

Reference27 articles.

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