Fe-Ti oxide micro-inclusions in clinopyroxene of oceanic gabbro: Phase content, orientation relations and petrogenetic implication

Author:

Ageeva Olga,Habler Gerlinde,Pertsev Alexey,Abart Rainer

Funder

Austrian Science foundation

Russian Foundation for Basic Research

IGEM RAS

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference56 articles.

1. Deformation of Fe-Ti oxides in gabbroic shear zones from the MARK area;Agar;Proceeding of the Ocean Drilling Program, Scientific Results,1997

2. Plagioclase hosted Fe-Ti-oxide micro-inclusions in an oceanic gabbro-plagiogranite association from the Mid Atlantic ridge at 13° 34′N;Ageeva;American Journal of Science,2016

3. Clouded plagioclase in metadolerite dikes, southeastern Bighorn Mountains, Wyoming;Amburstmacher;American Mineralogist,1974

4. Rutile solubility in H2O, H2O–SiO2, and H2O–NaAlSi3O8 fluids at 0.7–2.0GPa and 700–1000°C: implications for mobility of nominally insoluble elements;Antignano;Chemical Geology,2008

5. Direct observation of a section through slow-spreading oceanic crust;Auzende;Nature,1989

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