Ontology type: schema:ScholarlyArticle
1991-06
AUTHORSWilliam M. Lamb, Philip E. Brown, John W. Valley
ABSTRACTInvestigation of fluid inclusions in granitic and cale-silicate gneisses from the Adirondack Mountains, New York, has revealed the presence of various types, including: (1) CO2-rich, (2) mixed H2O−CO2±salt and (3) aqueous inclusions with no visible CO2. Many, if not all, of these inclusions were trapped or modified after the peak of granulite facies metamorphism, as shown by textural relations or by the lack of agreement between the composition of the fluids found in some inclusions and the composition of the peak-metamorphic fluid as estimated from mineral equilibria. Many fluid inclusions record conditions attained during retrograde cooling and uplift, with minimum pressures and temperatures of 2 to 3 kbar and 200 to 300°C. The temperatures and pressures derived from the investigation of these inclusions constrain the retrograde P-T path, and the results indicate that a period of cooling with little or no decompression. More... »
PAGES472-483
http://scigraph.springernature.com/pub.10.1007/bf00310681
DOIhttp://dx.doi.org/10.1007/bf00310681
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curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/bf00310681'
RDF/XML is a standard XML format for linked data.
curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/bf00310681'
This table displays all metadata directly associated to this object as RDF triples.
251 TRIPLES
21 PREDICATES
80 URIs
19 LITERALS
7 BLANK NODES