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Evaporite-bearing orogenic belts produce ligand-rich and diverse metamorphic fluids

Geochimica et cosmochimica acta, 2020-04, Vol.275, p.163-187

2020

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Stable Isotopic Evidence for Limited Fluid Flow through Dolomitic Marble in the Adamello Contact Aureole, Cima Uzza, Italy

Journal of petrology, 1999-06, Vol.40 (6), p.853

1999

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Deformed pillow lavas from the Central Hohe Tauern, Austria, and their bearing on the origin of epidote-banded greenstones

Earth and planetary science letters, 1979-01, Vol.43 (3), p.397-405

1979

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P–T–t Evolution of Ultrahigh-Temperature Granulites from the Saxon Granulite Massif, Germany. Part II: Geochronology

Journal of petrology, 2001-11, Vol.42 (11), p.2015-2032

2001

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Metamorphism and crustal rheology—implications for the structural development of the continental crust during prograde metamorphism

Geological Society special publication, 1986-01, Vol.24 (1), p.95-106

Weber, K.

1986

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EVIDENCE BEARING ON THE ORIGIN OF THE BELLEORAM STOCK, SOUTHERN NEWFOUNDLAND

Canadian journal of earth sciences, 1967-06, Vol.4 (3), p.413-431

1967

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A metamorphogenic alteration zone around the stratiform Broken Hill ore deposits, Australia

GEOCHEMICAL JOURNAL, 1975/12/20, Vol.9(4), pp.211-220

Plimer, I. R.

1975

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Evaporite-bearing orogenic belts produce ligand-rich and diverse metamorphic fluids

Stable Isotopic Evidence for Limited Fluid Flow through Dolomitic Marble in the Adamello Contact Aureole, Cima Uzza, Italy

Deformed pillow lavas from the Central Hohe Tauern, Austria, and their bearing on the origin of epidote-banded greenstones

P–T–t Evolution of Ultrahigh-Temperature Granulites from the Saxon Granulite Massif, Germany. Part II: Geochronology

Metamorphism and crustal rheology—implications for the structural development of the continental crust during prograde metamorphism

EVIDENCE BEARING ON THE ORIGIN OF THE BELLEORAM STOCK, SOUTHERN NEWFOUNDLAND

A metamorphogenic alteration zone around the stratiform Broken Hill ore deposits, Australia

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