Ontology type: schema:ScholarlyArticle
1995-07
AUTHORSD. P. Carrington, S. L. Harley
ABSTRACTPetrogenetic grids are a powerful tool for understanding metamorphic terrains and many theoretical grids have been suggested for the process of granulite formation in metapelitic rocks, via fluid-absent biotite melting reactions. However, application of these grids has been difficult due to the lack of suitable experimental constraints. We present here an experimentally determined and tightly constrained petrogenetic grid for KFMASH system metapelites which extends from 840–1000°C and 5.0–12.5 kbar. Sixty four experiments on three KFMASH, mineral-mix, bulk compositions (XMg=0.62, 0.74, 0.86) provide phase composition and assemblage data from which a grid can be derived and constrained. Reversal experiments and consideration of the phase composition data show the experiments to be close to equilibrium. The KFMASH univariant fluid-absent biotite melting reactions occur between 850 and 870°C at 5 kbar and between 900 and 915°C at 10 kbar. These reactions are connected to equilibria beyond the stability of biotite to develop a fixed framework within which the phase assemblage evolution of metapelitic rocks can be interpreted. The effect of minor components on phase equilibria is evaluated using the experimentally determined grid as a simple-system reference. The temperature at which melting occurs in metapelites is strongly controlled by the concentrations of titanium and fluorine in biotite. Pressure-temperature pseudosections presented for each of the experimental compositions show both the univariant and divariant reactions available to a particular bulk composition, clearly illustrating the possible evolution of the phase assemblage. The pseudosections also constrain the stability limits of More... »
PAGES270-291
http://scigraph.springernature.com/pub.10.1007/bf00306508
DOIhttp://dx.doi.org/10.1007/bf00306508
DIMENSIONShttps://app.dimensions.ai/details/publication/pub.1011413483
JSON-LD is the canonical representation for SciGraph data.
TIP: You can open this SciGraph record using an external JSON-LD service: JSON-LD Playground Google SDTT
[
{
"@context": "https://springernature.github.io/scigraph/jsonld/sgcontext.json",
"about": [
{
"id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/04",
"inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/",
"name": "Earth Sciences",
"type": "DefinedTerm"
},
{
"id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/0403",
"inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/",
"name": "Geology",
"type": "DefinedTerm"
}
],
"author": [
{
"affiliation": {
"alternateName": "Department of Geology and Geophysics, University of Edinburgh, West Mains Road, EH9 3JW, Edinburgh, Scotland, UK",
"id": "http://www.grid.ac/institutes/grid.4305.2",
"name": [
"Department of Geology and Geophysics, University of Edinburgh, West Mains Road, EH9 3JW, Edinburgh, Scotland, UK"
],
"type": "Organization"
},
"familyName": "Carrington",
"givenName": "D. P.",
"id": "sg:person.015760141547.57",
"sameAs": [
"https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.015760141547.57"
],
"type": "Person"
},
{
"affiliation": {
"alternateName": "Department of Geology and Geophysics, University of Edinburgh, West Mains Road, EH9 3JW, Edinburgh, Scotland, UK",
"id": "http://www.grid.ac/institutes/grid.4305.2",
"name": [
"Department of Geology and Geophysics, University of Edinburgh, West Mains Road, EH9 3JW, Edinburgh, Scotland, UK"
],
"type": "Organization"
},
"familyName": "Harley",
"givenName": "S. L.",
"id": "sg:person.01275544350.30",
"sameAs": [
"https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.01275544350.30"
],
"type": "Person"
}
],
"citation": [
{
"id": "sg:pub.10.1007/bf00372150",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1039488171",
"https://doi.org/10.1007/bf00372150"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/978-94-015-3929-6_2",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1044474150",
"https://doi.org/10.1007/978-94-015-3929-6_2"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf01046539",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1026716128",
"https://doi.org/10.1007/bf01046539"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00374063",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1042381468",
"https://doi.org/10.1007/bf00374063"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/978-3-642-88097-1_8",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1013421715",
"https://doi.org/10.1007/978-3-642-88097-1_8"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/978-94-015-3929-6_4",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1052571680",
"https://doi.org/10.1007/978-94-015-3929-6_4"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00310707",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1027201341",
"https://doi.org/10.1007/bf00310707"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00380171",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1042074493",
"https://doi.org/10.1007/bf00380171"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00382571",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1021612662",
"https://doi.org/10.1007/bf00382571"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/978-94-015-3929-6_12",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1053592148",
"https://doi.org/10.1007/978-94-015-3929-6_12"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00371463",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1040607391",
"https://doi.org/10.1007/bf00371463"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00373879",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1039605524",
"https://doi.org/10.1007/bf00373879"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00372231",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1046616704",
"https://doi.org/10.1007/bf00372231"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00374721",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1043992273",
"https://doi.org/10.1007/bf00374721"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00387203",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1013616864",
"https://doi.org/10.1007/bf00387203"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00375178",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1044244054",
"https://doi.org/10.1007/bf00375178"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf01187140",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1013412604",
"https://doi.org/10.1007/bf01187140"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00572165",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1009239489",
"https://doi.org/10.1007/bf00572165"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/978-94-011-6496-2",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1011961561",
"https://doi.org/10.1007/978-94-011-6496-2"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/bf00307326",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1012274478",
"https://doi.org/10.1007/bf00307326"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/978-1-4613-2347-1_3",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1010594200",
"https://doi.org/10.1007/978-1-4613-2347-1_3"
],
"type": "CreativeWork"
},
{
"id": "sg:pub.10.1007/978-94-015-3929-6_5",
"sameAs": [
"https://app.dimensions.ai/details/publication/pub.1000668743",
"https://doi.org/10.1007/978-94-015-3929-6_5"
],
"type": "CreativeWork"
}
],
"datePublished": "1995-07",
"datePublishedReg": "1995-07-01",
"description": "Petrogenetic grids are a powerful tool for understanding metamorphic terrains and many theoretical grids have been suggested for the process of granulite formation in metapelitic rocks, via fluid-absent biotite melting reactions. However, application of these grids has been difficult due to the lack of suitable experimental constraints. We present here an experimentally determined and tightly constrained petrogenetic grid for KFMASH system metapelites which extends from 840\u20131000\u00b0C and 5.0\u201312.5 kbar. Sixty four experiments on three KFMASH, mineral-mix, bulk compositions (XMg=0.62, 0.74, 0.86) provide phase composition and assemblage data from which a grid can be derived and constrained. Reversal experiments and consideration of the phase composition data show the experiments to be close to equilibrium. The KFMASH univariant fluid-absent biotite melting reactions occur between 850 and 870\u00b0C at 5 kbar and between 900 and 915\u00b0C at 10 kbar. These reactions are connected to equilibria beyond the stability of biotite to develop a fixed framework within which the phase assemblage evolution of metapelitic rocks can be interpreted. The effect of minor components on phase equilibria is evaluated using the experimentally determined grid as a simple-system reference. The temperature at which melting occurs in metapelites is strongly controlled by the concentrations of titanium and fluorine in biotite. Pressure-temperature pseudosections presented for each of the experimental compositions show both the univariant and divariant reactions available to a particular bulk composition, clearly illustrating the possible evolution of the phase assemblage. The pseudosections also constrain the stability limits of",
"genre": "article",
"id": "sg:pub.10.1007/bf00306508",
"isAccessibleForFree": false,
"isPartOf": [
{
"id": "sg:journal.1026106",
"issn": [
"0010-7999",
"1432-0967"
],
"name": "Contributions to Mineralogy and Petrology",
"publisher": "Springer Nature",
"type": "Periodical"
},
{
"issueNumber": "3-4",
"type": "PublicationIssue"
},
{
"type": "PublicationVolume",
"volumeNumber": "120"
}
],
"keywords": [
"petrogenetic grid",
"metapelitic rocks",
"bulk composition",
"pressure\u2013temperature pseudosections",
"high-grade metapelites",
"stability of biotite",
"phase assemblage evolution",
"granulite formation",
"partial melting",
"metamorphic terrains",
"KFMASH system",
"divariant reactions",
"assemblage data",
"biotite",
"metapelites",
"phase assemblage",
"kbar",
"pseudosections",
"rocks",
"composition data",
"phase relations",
"experimental constraints",
"concentration of titanium",
"phase composition data",
"composition",
"minor components",
"reversal experiments",
"KFMASH",
"possible evolution",
"evolution",
"assemblages",
"melting",
"terrain",
"theoretical grid",
"phase equilibria",
"equilibrium",
"grid",
"data",
"powerful tool",
"formation",
"temperature",
"constraints",
"concentration",
"experimental compositions",
"experiments",
"fluorine",
"stability limit",
"process",
"components",
"limit",
"lack",
"relation",
"system",
"phase composition",
"reference",
"framework",
"consideration",
"tool",
"effect",
"reaction",
"stability",
"titanium",
"applications"
],
"name": "Partial melting and phase relations in high-grade metapelites: an experimental petrogenetic grid in the KFMASH system",
"pagination": "270-291",
"productId": [
{
"name": "dimensions_id",
"type": "PropertyValue",
"value": [
"pub.1011413483"
]
},
{
"name": "doi",
"type": "PropertyValue",
"value": [
"10.1007/bf00306508"
]
}
],
"sameAs": [
"https://doi.org/10.1007/bf00306508",
"https://app.dimensions.ai/details/publication/pub.1011413483"
],
"sdDataset": "articles",
"sdDatePublished": "2022-08-04T16:52",
"sdLicense": "https://scigraph.springernature.com/explorer/license/",
"sdPublisher": {
"name": "Springer Nature - SN SciGraph project",
"type": "Organization"
},
"sdSource": "s3://com-springernature-scigraph/baseset/20220804/entities/gbq_results/article/article_305.jsonl",
"type": "ScholarlyArticle",
"url": "https://doi.org/10.1007/bf00306508"
}
]Download the RDF metadata as: json-ld nt turtle xml License info
JSON-LD is a popular format for linked data which is fully compatible with JSON.
curl -H 'Accept: application/ld+json' 'https://scigraph.springernature.com/pub.10.1007/bf00306508'
N-Triples is a line-based linked data format ideal for batch operations.
curl -H 'Accept: application/n-triples' 'https://scigraph.springernature.com/pub.10.1007/bf00306508'
Turtle is a human-readable linked data format.
curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/bf00306508'
RDF/XML is a standard XML format for linked data.
curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/bf00306508'
This table displays all metadata directly associated to this object as RDF triples.
215 TRIPLES
21 PREDICATES
110 URIs
80 LITERALS
6 BLANK NODES