Garnet growth as a proxy for progressive subduction zone dehydration Ethan F. Baxter1 and Mark J. Caddick2 1 Department of Earth - Borneo peat swamp forests - Document - PDFSEARCH.IO

First Page		Document Content
Date: 2014-11-05 20:34:56 Metamorphic petrology Lawsonite Subduction zone metamorphism Eclogite Blueschist Metamorphism Subduction Porphyroblast Garnet Amphibolite Basalt Mineral		Garnet growth as a proxy for progressive subduction zone dehydration Ethan F. Baxter1 and Mark J. Caddick2 1 Department of Earth & Environment, Boston University, 675 Commonwealth Avenue, Boston, Massachusetts 02215, US Add to Reading List Source URL: www.metamorphism.geos.vt.edu Download Document from Source Website File Size: 174,36 KB Share Document on Facebook

	MINERALOGICAL SOCIETY (LONDON) A meeting of the Society was held on Thursday, January 22nd,1953, at 5 n.u., in the apartments of the Geological Society of London, Burlington House, piccadilly, W.1 (by kind permission). T DocID: 1q1eM - View Document
	Beyond the equilibrium paradigm: How consideration of kinetics enhances metamorphic interpretation DocID: 1pXdI - View Document
	American Mineralogist, Volume 77, pages, 1992 NEW MINERAL NAMES* JorrN L. J.q.Nrnon CANMET, 555 Booth Street,Ottawa,Ontario KIA 0Gl, Canada DocID: 1pqF9 - View Document
	Pulsed dehydration and garnet growth during subduction revealed by zoned garnet geochronology and thermodynamic modeling, Sifnos, Greece DocID: 1oWj7 - View Document
	Garnet growth as a proxy for progressive subduction zone dehydration Ethan F. Baxter1 and Mark J. Caddick2 1 Department of Earth & Environment, Boston University, 675 Commonwealth Avenue, Boston, Massachusetts 02215, US DocID: 1oLrT - View Document