Fluid-Rock Interaction in the Miocene, Post-Caldera, Tejeda Intrusive Complex, Gran Canaria (Canary Islands): Insights from Mineralogy, and O- and H-Isotope Geochemistry-Reference-Cited by-同舟云学术

Fluid-Rock Interaction in the Miocene, Post-Caldera, Tejeda Intrusive Complex, Gran Canaria (Canary Islands): Insights from Mineralogy, and O- and H-Isotope Geochemistry

Published:2010-09-21 Issue:10 Volume:51 Page:2149-2176
ISSN:0022-3530
Container-title:Journal of Petrology
language:en
Short-container-title:Journal of Petrology

Author:

Donoghue E.,Troll V. R.,Harris C.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/51/10/2149/4482705/egq052.pdf

Reference119 articles.

1. Composition and evolution of submarine volcanic rocks from the central and western Canary Islands

2. Stable isotopes and amphibole chemistry on hydrothermally altered granitoids in the North Chilean Precordillera: a limited role for meteoric water?

3. Evolution of the Cañadas edifice and its implications for the origin of the Cañadas Caldera (Tenerife, Canary Islands)

4. Direct evidence for the origin of low-18O silicic magmas: quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake, Oregon

5. Formation of low-δ18O rhyolites after caldera collapse at Yellowstone, Wyoming, USA

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1. Silicic frothy xenoliths (xeno-pumice) in recent volcanics from Gran Canaria, Canary Islands;Journal of Volcanology and Geothermal Research;2023-08

2. The explosive-effusive transition within the Miocene Fataga suite, Gran Canaria;Chemical Geology;2023-01

3. Generation and Field Relations of Low-δ18O Silica-Undersaturated and Mildly Saturated Alkaline Magmas: a Case Study from the Fataga Group, Gran Canaria;Journal of Petrology;2022-09-01

4. Whole-rock oxygen isotope ratios as a proxy for the strength and stiffness of hydrothermally altered volcanic rocks;Bulletin of Volcanology;2022-07-15

5. Absence of hydrothermal oxygen isotope variations in host rocks supports magmatic origin of the giant Grängesberg iron oxide–apatite (IOA) deposit, Central Sweden;International Journal of Earth Sciences;2021-11-13