Absence of low-δ18O magmas despite widespread assimilation of altered crust in a large magmatic and hydrothermal province

Author:

Rooyakkers Shane M.ORCID,Chambefort Isabelle,Faure KevinORCID,Wilson Colin J.N.ORCID,Barker Simon J.,Mortimer Nick,Elms Hannah C.ORCID,Troch JulianaORCID,Charlier Bruce L.A.,Leonard Graham S.ORCID,Farsky DavidORCID

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference82 articles.

1. Absar, A., 1988. Oxygen isotope and hydrothermal alteration studies at Kawerau and Ohaaki-Broadlands geothermal fields, New Zealand. Ph.D. thesis, University of Auckland, Auckland, New Zealand.

2. Absar, A., Blattner, P., 1985. Successive hydrothermal events, as indicated by oxygen isotope composition and petrography of greywacke basement rocks, Kawerau geothermal field, New Zealand. In: Proc. 7th N.Z. Geotherm. Workshop, Auckland, New Zealand.

3. Low-18O silicic magmas: why are they so rare?;Balsley;Earth Planet. Sci. Lett.,1998

4. What lies beneath? Reconstructing the primitive magmas fueling voluminous silicic volcanism using olivine-hosted melt inclusions;Barker;Geology,2020

5. Geophysical evidence on the structure of the Taupo Volcanic Zone and its hydrothermal circulation;Bibby;J. Volcanol. Geotherm. Res.,1995

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