Petrogenesis of basaltic rocks from the Mariana Trough

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1981

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University of Hawaii at Manoa

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The Mariana Trough, a young, actively spreading back-arc bas in, 1s very similar tectonically to normal mid-ocean ridges. The major difference 1s proximity of the spreading center 1n the Mariana Trough to an active subduction zone. Basaltic glasses retrie

Description

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Basalt, Petrology--Mariana Islands., Island arcs--Mariana Islands., Basalt--Mariana Islands.

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North Pacific Ocean--Mariana Trench

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Theses for the degree of Doctor of Philosophy (University of Hawaii at Manoa). Geology and Geophysics

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Table of Contents

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