Tectonic and magmatic evolution of the southernmost Mariana convergent margin: Constraints from geochronology and geochemistry of the Challenger Deep sediments-Reference-Cited by-同舟云学术

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Tectonic and magmatic evolution of the southernmost Mariana convergent margin: Constraints from geochronology and geochemistry of the Challenger Deep sediments

Published:2024-12 Issue: Volume:488-489 Page:107796
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Yang Ming,Wu Tao,Zhang Wen,Tian Liyan,Lu Jianggu,Song Taoran,Zhu Hengrui,Hong Yidi,Chen Jiawang

Funder

National Natural Science Foundation of China

Hainan Province Natural Science Foundation

Publisher

Elsevier BV

Reference74 articles.

1. Time scales of tectonic landscapes and their sediment routing systems;Allen;Geol. Soc. Lond. Spec. Publ.,2008

2. Clinopyroxene composition of ophiolite basalts as petrogenetic indicator;Beccaluva;Chem. Geol.,1989

3. Magnetostratigraphic evidence for deep-sea erosion on the Pacific Plate, south of Mariana Trench, since the middle Pleistocene: potential constraints for Antarctic bottom water circulation;Deng;Int. Geol. Rev.,2016

4. Geology, environment, and life in the deepest part of the world’s oceans;Du;The Innovation,2021

5. The mean composition of ocean ridge basalts;Gale;Geochem. Geophys. Geosyst.,2013

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