Zircon double-dating, trace element and O isotope analysis to decipher late Pleistocene explosive-effusive eruptions from a zoned ocean-island magma system, Ascension Island

Author:

Scarrow Jane H.ORCID,Schmitt Axel K.ORCID,Danišík Martin,Chamberlain Katy J.ORCID,Davies Bridie V.ORCID,Rushton Jeremy,Brown Richard J.,Barclay Jenni

Funder

Universität Heidelberg

Universidad de Granada

H2020 Marie Skłodowska-Curie Actions

Horizon 2020

European Commission

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference87 articles.

1. Chemistry of fluids from ascension #1, a deep geothermal well on Ascension Island, South Atlantic Ocean;Adams;Geothermics,1996

2. Hafnium;Ahrens,1969

3. 39Ar-40Ar dating: the importance of K-feldspars on multi-mineral data of polyorogenic areas;Albarede;J. Geol.,1978

4. Zircon crystallization and recycling in the magma chamber of the rhyolitic Kos Plateau Tuff (Aegean arc);Bachmann;Geology,2007

5. Magmatic processes at Snæfell Volcano, Iceland, constrained by zircon ages, isotopes, and trace elements;Banik;G-cubed,2021

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