Geothermometry and geobarometry of plagioclase-hornblende bearing assemblages View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1982-09

AUTHORS

L. P. Plyusnina

ABSTRACT

The reaction Hb+Zo(Ep)+H2O+CO2⇌Pl+ Chl+Cc+Q was studied under hydrothermal conditions at Ptotal=2, 4, 6 and 8 kb at . The continious transition from tremolite (actinolite) to Al-rich hornblende was fixed along the equilibrium curve of the reaction, providing a complete solid solution in the calcic amphibole series. A dependence of Al content in Ca-amphiboles and coexisting plagioclases on PT-conditions of their crystallization, determined for a wide range of temperature (450–650° C) and pressure (2–8 kb), has been used for construction of the experimental geothermobarometer. This may be employed to deduce temperature and pressure conditions of metamorphism of the albite-epidote-amphibolite and the amphibolite facies metabasites, including zoisite (or epidote)-bearing assemblages. An application of the Hb-Pl geothermobarometer is illustrated on the Patom Highland amphibolites and also on the well-known mafic schists of Vermont. More... »

PAGES

140-146

References to SciGraph publications

  • 1974-09. Al and Ti contents of hornblende, indicators of pressure and temperature of regional metamorphism in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1980-09. The assemblage orthopyroxene+cummingtonite+quartz. The low-temperature stability limit in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1975-06. Actinolite-hornblende pairs in metamorphosed gabbros, Hidaka mountains, Hokkaido in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1974-09. Metabasite amphiboles of the Scottish Dalradian in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1007/bf00374891

    DOI

    http://dx.doi.org/10.1007/bf00374891

    DIMENSIONS

    https://app.dimensions.ai/details/publication/pub.1016994235


    Indexing Status Check whether this publication has been indexed by Scopus and Web Of Science using the SN Indexing Status Tool
    Incoming Citations Browse incoming citations for this publication using opencitations.net

    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/2008/0299", 
            "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
            "name": "Other Physical Sciences", 
            "type": "DefinedTerm"
          }, 
          {
            "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/02", 
            "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
            "name": "Physical Sciences", 
            "type": "DefinedTerm"
          }
        ], 
        "author": [
          {
            "affiliation": {
              "name": [
                "Institute of Experimental Mineralogy, USSR Acad. Sci., 142432, Chernogolovka, Moscow, District, USSR"
              ], 
              "type": "Organization"
            }, 
            "familyName": "Plyusnina", 
            "givenName": "L. P.", 
            "type": "Person"
          }
        ], 
        "citation": [
          {
            "id": "https://doi.org/10.1016/0024-4937(78)90001-4", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1007280356"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0024-4937(78)90001-4", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1007280356"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00371537", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1015876244", 
              "https://doi.org/10.1007/bf00371537"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00371537", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1015876244", 
              "https://doi.org/10.1007/bf00371537"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00383440", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1024979251", 
              "https://doi.org/10.1007/bf00383440"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00383440", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1024979251", 
              "https://doi.org/10.1007/bf00383440"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00373856", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1041197883", 
              "https://doi.org/10.1007/bf00373856"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00373856", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1041197883", 
              "https://doi.org/10.1007/bf00373856"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00376633", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1041697257", 
              "https://doi.org/10.1007/bf00376633"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00376633", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1041697257", 
              "https://doi.org/10.1007/bf00376633"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.2343/geochemj.11.253", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1043236710"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1093/petrology/13.3.457", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1059972311"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1093/petrology/21.1.1-a", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1059972497"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.2475/ajs.274.6.613", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1070841158"
            ], 
            "type": "CreativeWork"
          }
        ], 
        "datePublished": "1982-09", 
        "datePublishedReg": "1982-09-01", 
        "description": "The reaction Hb+Zo(Ep)+H2O+CO2\u21ccPl+ Chl+Cc+Q was studied under hydrothermal conditions at Ptotal=2, 4, 6 and 8 kb at . The continious transition from tremolite (actinolite) to Al-rich hornblende was fixed along the equilibrium curve of the reaction, providing a complete solid solution in the calcic amphibole series. A dependence of Al content in Ca-amphiboles and coexisting plagioclases on PT-conditions of their crystallization, determined for a wide range of temperature (450\u2013650\u00b0 C) and pressure (2\u20138 kb), has been used for construction of the experimental geothermobarometer. This may be employed to deduce temperature and pressure conditions of metamorphism of the albite-epidote-amphibolite and the amphibolite facies metabasites, including zoisite (or epidote)-bearing assemblages. An application of the Hb-Pl geothermobarometer is illustrated on the Patom Highland amphibolites and also on the well-known mafic schists of Vermont.", 
        "genre": "research_article", 
        "id": "sg:pub.10.1007/bf00374891", 
        "inLanguage": [
          "en"
        ], 
        "isAccessibleForFree": false, 
        "isPartOf": [
          {
            "id": "sg:journal.1026106", 
            "issn": [
              "0010-7999", 
              "1432-0967"
            ], 
            "name": "Contributions to Mineralogy and Petrology", 
            "type": "Periodical"
          }, 
          {
            "issueNumber": "2", 
            "type": "PublicationIssue"
          }, 
          {
            "type": "PublicationVolume", 
            "volumeNumber": "80"
          }
        ], 
        "name": "Geothermometry and geobarometry of plagioclase-hornblende bearing assemblages", 
        "pagination": "140-146", 
        "productId": [
          {
            "name": "doi", 
            "type": "PropertyValue", 
            "value": [
              "10.1007/bf00374891"
            ]
          }, 
          {
            "name": "readcube_id", 
            "type": "PropertyValue", 
            "value": [
              "50f7c4e4daf3fbe423c581189882f3cac494e1e23a9cdb9be76d775cfad329ce"
            ]
          }, 
          {
            "name": "dimensions_id", 
            "type": "PropertyValue", 
            "value": [
              "pub.1016994235"
            ]
          }
        ], 
        "sameAs": [
          "https://doi.org/10.1007/bf00374891", 
          "https://app.dimensions.ai/details/publication/pub.1016994235"
        ], 
        "sdDataset": "articles", 
        "sdDatePublished": "2019-04-15T08:49", 
        "sdLicense": "https://scigraph.springernature.com/explorer/license/", 
        "sdPublisher": {
          "name": "Springer Nature - SN SciGraph project", 
          "type": "Organization"
        }, 
        "sdSource": "s3://com-uberresearch-data-dimensions-target-20181106-alternative/cleanup/v134/2549eaecd7973599484d7c17b260dba0a4ecb94b/merge/v9/a6c9fde33151104705d4d7ff012ea9563521a3ce/jats-lookup/v90/0000000374_0000000374/records_119727_00000000.jsonl", 
        "type": "ScholarlyArticle", 
        "url": "http://link.springer.com/10.1007/BF00374891"
      }
    ]
     

    Download the RDF metadata as:  json-ld nt turtle xml License info

    HOW TO GET THIS DATA PROGRAMMATICALLY:

    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/bf00374891'

    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/bf00374891'

    Turtle is a human-readable linked data format.

    curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/bf00374891'

    RDF/XML is a standard XML format for linked data.

    curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/bf00374891'


     

    This table displays all metadata directly associated to this object as RDF triples.

    90 TRIPLES      21 PREDICATES      36 URIs      19 LITERALS      7 BLANK NODES

    Subject Predicate Object
    1 sg:pub.10.1007/bf00374891 schema:about anzsrc-for:02
    2 anzsrc-for:0299
    3 schema:author N9fc03be738af44b1b61f136153948ee7
    4 schema:citation sg:pub.10.1007/bf00371537
    5 sg:pub.10.1007/bf00373856
    6 sg:pub.10.1007/bf00376633
    7 sg:pub.10.1007/bf00383440
    8 https://doi.org/10.1016/0024-4937(78)90001-4
    9 https://doi.org/10.1093/petrology/13.3.457
    10 https://doi.org/10.1093/petrology/21.1.1-a
    11 https://doi.org/10.2343/geochemj.11.253
    12 https://doi.org/10.2475/ajs.274.6.613
    13 schema:datePublished 1982-09
    14 schema:datePublishedReg 1982-09-01
    15 schema:description The reaction Hb+Zo(Ep)+H2O+CO2⇌Pl+ Chl+Cc+Q was studied under hydrothermal conditions at Ptotal=2, 4, 6 and 8 kb at . The continious transition from tremolite (actinolite) to Al-rich hornblende was fixed along the equilibrium curve of the reaction, providing a complete solid solution in the calcic amphibole series. A dependence of Al content in Ca-amphiboles and coexisting plagioclases on PT-conditions of their crystallization, determined for a wide range of temperature (450–650° C) and pressure (2–8 kb), has been used for construction of the experimental geothermobarometer. This may be employed to deduce temperature and pressure conditions of metamorphism of the albite-epidote-amphibolite and the amphibolite facies metabasites, including zoisite (or epidote)-bearing assemblages. An application of the Hb-Pl geothermobarometer is illustrated on the Patom Highland amphibolites and also on the well-known mafic schists of Vermont.
    16 schema:genre research_article
    17 schema:inLanguage en
    18 schema:isAccessibleForFree false
    19 schema:isPartOf N004ae62b552144cf8af3cd660d53bacd
    20 N1cf14df2215448e696cb2c1021b9de6c
    21 sg:journal.1026106
    22 schema:name Geothermometry and geobarometry of plagioclase-hornblende bearing assemblages
    23 schema:pagination 140-146
    24 schema:productId N45e8ec04d31e4cfcb1bff35d15ab04d2
    25 N4c6c8f35c7454ecd916a0d25c2f27d76
    26 N53032e854d204f47a2056af6b2bd0d53
    27 schema:sameAs https://app.dimensions.ai/details/publication/pub.1016994235
    28 https://doi.org/10.1007/bf00374891
    29 schema:sdDatePublished 2019-04-15T08:49
    30 schema:sdLicense https://scigraph.springernature.com/explorer/license/
    31 schema:sdPublisher N46a9e0eb1e7c414fb73fed6808b37c5c
    32 schema:url http://link.springer.com/10.1007/BF00374891
    33 sgo:license sg:explorer/license/
    34 sgo:sdDataset articles
    35 rdf:type schema:ScholarlyArticle
    36 N004ae62b552144cf8af3cd660d53bacd schema:volumeNumber 80
    37 rdf:type schema:PublicationVolume
    38 N0cfc54133de64795bc5ab532c9311820 schema:affiliation N852b06ed18cc4b608a208c4015a9820e
    39 schema:familyName Plyusnina
    40 schema:givenName L. P.
    41 rdf:type schema:Person
    42 N1cf14df2215448e696cb2c1021b9de6c schema:issueNumber 2
    43 rdf:type schema:PublicationIssue
    44 N45e8ec04d31e4cfcb1bff35d15ab04d2 schema:name doi
    45 schema:value 10.1007/bf00374891
    46 rdf:type schema:PropertyValue
    47 N46a9e0eb1e7c414fb73fed6808b37c5c schema:name Springer Nature - SN SciGraph project
    48 rdf:type schema:Organization
    49 N4c6c8f35c7454ecd916a0d25c2f27d76 schema:name dimensions_id
    50 schema:value pub.1016994235
    51 rdf:type schema:PropertyValue
    52 N53032e854d204f47a2056af6b2bd0d53 schema:name readcube_id
    53 schema:value 50f7c4e4daf3fbe423c581189882f3cac494e1e23a9cdb9be76d775cfad329ce
    54 rdf:type schema:PropertyValue
    55 N852b06ed18cc4b608a208c4015a9820e schema:name Institute of Experimental Mineralogy, USSR Acad. Sci., 142432, Chernogolovka, Moscow, District, USSR
    56 rdf:type schema:Organization
    57 N9fc03be738af44b1b61f136153948ee7 rdf:first N0cfc54133de64795bc5ab532c9311820
    58 rdf:rest rdf:nil
    59 anzsrc-for:02 schema:inDefinedTermSet anzsrc-for:
    60 schema:name Physical Sciences
    61 rdf:type schema:DefinedTerm
    62 anzsrc-for:0299 schema:inDefinedTermSet anzsrc-for:
    63 schema:name Other Physical Sciences
    64 rdf:type schema:DefinedTerm
    65 sg:journal.1026106 schema:issn 0010-7999
    66 1432-0967
    67 schema:name Contributions to Mineralogy and Petrology
    68 rdf:type schema:Periodical
    69 sg:pub.10.1007/bf00371537 schema:sameAs https://app.dimensions.ai/details/publication/pub.1015876244
    70 https://doi.org/10.1007/bf00371537
    71 rdf:type schema:CreativeWork
    72 sg:pub.10.1007/bf00373856 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041197883
    73 https://doi.org/10.1007/bf00373856
    74 rdf:type schema:CreativeWork
    75 sg:pub.10.1007/bf00376633 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041697257
    76 https://doi.org/10.1007/bf00376633
    77 rdf:type schema:CreativeWork
    78 sg:pub.10.1007/bf00383440 schema:sameAs https://app.dimensions.ai/details/publication/pub.1024979251
    79 https://doi.org/10.1007/bf00383440
    80 rdf:type schema:CreativeWork
    81 https://doi.org/10.1016/0024-4937(78)90001-4 schema:sameAs https://app.dimensions.ai/details/publication/pub.1007280356
    82 rdf:type schema:CreativeWork
    83 https://doi.org/10.1093/petrology/13.3.457 schema:sameAs https://app.dimensions.ai/details/publication/pub.1059972311
    84 rdf:type schema:CreativeWork
    85 https://doi.org/10.1093/petrology/21.1.1-a schema:sameAs https://app.dimensions.ai/details/publication/pub.1059972497
    86 rdf:type schema:CreativeWork
    87 https://doi.org/10.2343/geochemj.11.253 schema:sameAs https://app.dimensions.ai/details/publication/pub.1043236710
    88 rdf:type schema:CreativeWork
    89 https://doi.org/10.2475/ajs.274.6.613 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070841158
    90 rdf:type schema:CreativeWork
     




    Preview window. Press ESC to close (or click here)


    ...