Silica activity and Ptotal in igneous rocks View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1971-03

AUTHORS

J. Nicholls, I. S. E. Carmichael, J. C. Stormer

ABSTRACT

The variation of silica activity with temperature and pressure for a variety of silica buffers (mineral pairs) allows Ptotal to be calculated for a wide range of igneous rocks. The method also depends on evaluating (∂ log aSiO2/∂P)T and (Δ log aSiO2/ΔT)p; the former is equivalent to the partial molar volume of silica in silicate liquids, while the latter is estimated from published experiments on natural melts. Results for calc-alkaline rhyolites with phenocrysts of quartz, olivine or orthopyroxene, and iron-titanium oxides, range from 3.45 to 9.58 kilobars; a pantellerite is intermediate at 7.53 kilobars. At 1327° C, the silicate inclusions in diamond equilibrated at 63.5 kilobars, and the kimberlite crystallisation path intersected the baddeleyite-zircon reaction at 55.7 kilobars. Two trachybasalts would equilibrate with their lherzolite xenoliths at 17.0 and 21.0 kilobars at surface quenching temperatures. Potassic lavas such as orendites and ugandites at 1300° C would be in equilibrium with mantle olivine-orthropyroxene at 35.1 and 69.0 kilobars respectively. Basalts and basaltic-andesites could equilibrate (at 1100° C) with quartz at between 24.9 and 26.8 kilobars; quartz can therefore be considered a possible high pressure “xenocryst” in lavas with low Sr87/Sr86 ratios. Andesites will equilibrate at 1300° C with the mantle at a depth of 75 kilometres; at greater depths andesite will have a basaltic precursor. In general, lavas with low silica activity will equilibrate at greater depths in the mantle than those with higher silica activities. The Apollo 11 basalts contain minerals which suggest equilibration at 37 kilobars; the calculated quenching temperature is 1009° C, from which logfO2 can be derived (−15.2) which in turn indicates approximately 0.10% Fe2O3 in these lavas. More... »

PAGES

1-20

References to SciGraph publications

  • 1966-09. Ultramafic inclusions in basaltic rocks from Hawaii in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1970-12. The volcanoes and caldera of Talasea, New Britain: Mineralogy in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1967-03. The mineralogy and petrology of the volcanic rocks from the Leucite Hills, Wyoming in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1968-09. Quaternary lavas from the southern Cascades, western U.S.A. in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1971-06. Voluminous low temperature rhyolitic magmas in New Zealand in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1968-05. Genesis of the calc-alkaline igneous rock suite in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1966-03. The iron-titanium oxides of salic volcanic rocks and their associated ferromagnesian silicates in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1967-06. The genesis of basaltic magmas in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1007/bf00373791

    DOI

    http://dx.doi.org/10.1007/bf00373791

    DIMENSIONS

    https://app.dimensions.ai/details/publication/pub.1024667496


    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/2008/0403", 
            "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
            "name": "Geology", 
            "type": "DefinedTerm"
          }, 
          {
            "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"
          }
        ], 
        "author": [
          {
            "affiliation": {
              "alternateName": "University of Calgary", 
              "id": "https://www.grid.ac/institutes/grid.22072.35", 
              "name": [
                "Dept. of Geology, University of Calgary, Alberta, Canada"
              ], 
              "type": "Organization"
            }, 
            "familyName": "Nicholls", 
            "givenName": "J.", 
            "id": "sg:person.016604357276.36", 
            "sameAs": [
              "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.016604357276.36"
            ], 
            "type": "Person"
          }, 
          {
            "affiliation": {
              "alternateName": "University of California, Berkeley", 
              "id": "https://www.grid.ac/institutes/grid.47840.3f", 
              "name": [
                "Dept. of Geology and Geophysics, University of California, 94720, Berkeley, Calif."
              ], 
              "type": "Organization"
            }, 
            "familyName": "Carmichael", 
            "givenName": "I. S. E.", 
            "id": "sg:person.01157747754.50", 
            "sameAs": [
              "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.01157747754.50"
            ], 
            "type": "Person"
          }, 
          {
            "affiliation": {
              "alternateName": "University of Georgia", 
              "id": "https://www.grid.ac/institutes/grid.213876.9", 
              "name": [
                "Dept. of Geology, University of Georgia, 30601, Athens, Georgia"
              ], 
              "type": "Organization"
            }, 
            "familyName": "Stormer", 
            "givenName": "J. C.", 
            "id": "sg:person.01251612234.88", 
            "sameAs": [
              "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.01251612234.88"
            ], 
            "type": "Person"
          }
        ], 
        "citation": [
          {
            "id": "https://doi.org/10.1016/0031-9201(70)90063-4", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1007052186"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0031-9201(70)90063-4", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1007052186"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1002/gj.3350040105", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1010189291"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1017/s0080456800004798", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1010467576"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1029/jb073i006p02261", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1010859157"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1098/rsta.1972.0008", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1011930216"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1130/0016-7606(1970)81[311:sroqlo]2.0.co;2", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1014383871"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1029/jb074i022p05301", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1017380337"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1029/jz069i020p04377", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1019241559"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00390081", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1019967277", 
              "https://doi.org/10.1007/bf00390081"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00390081", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1019967277", 
              "https://doi.org/10.1007/bf00390081"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01167214", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1020017210", 
              "https://doi.org/10.1007/bf01167214"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf01167214", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1020017210", 
              "https://doi.org/10.1007/bf01167214"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00370985", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1022578692", 
              "https://doi.org/10.1007/bf00370985"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00370985", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1022578692", 
              "https://doi.org/10.1007/bf00370985"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00518082", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1025265667", 
              "https://doi.org/10.1007/bf00518082"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00518082", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1025265667", 
              "https://doi.org/10.1007/bf00518082"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1130/0016-7606(1970)81[17:tvacot]2.0.co;2", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1026021765"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00371806", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1028685359", 
              "https://doi.org/10.1007/bf00371806"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00371806", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1028685359", 
              "https://doi.org/10.1007/bf00371806"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00508912", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1039435514", 
              "https://doi.org/10.1007/bf00508912"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00508912", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1039435514", 
              "https://doi.org/10.1007/bf00508912"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1130/0016-7606(1970)81[39:srotts]2.0.co;2", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1039472297"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00372052", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1039651157", 
              "https://doi.org/10.1007/bf00372052"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00372052", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1039651157", 
              "https://doi.org/10.1007/bf00372052"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0016-7037(71)90081-0", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1047227336"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1016/0016-7037(71)90081-0", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1047227336"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00386111", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1048833295", 
              "https://doi.org/10.1007/bf00386111"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "sg:pub.10.1007/bf00386111", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1048833295", 
              "https://doi.org/10.1007/bf00386111"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1029/jb075i032p06480", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1050239594"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1086/626745", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1058822527"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1093/petrology/3.1.82", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1059972823"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1093/petrology/5.2.310", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1059973282"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1093/petrology/5.3.435", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1059973285"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.2113/gsecongeo.63.5.495", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1068929885"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.2475/ajs.269.2.132", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1070840859"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.2475/ajs.269.2.169", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1070840860"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.2475/ajs.270.5.334", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1070840915"
            ], 
            "type": "CreativeWork"
          }, 
          {
            "id": "https://doi.org/10.1130/spe132-p1", 
            "sameAs": [
              "https://app.dimensions.ai/details/publication/pub.1088804973"
            ], 
            "type": "CreativeWork"
          }
        ], 
        "datePublished": "1971-03", 
        "datePublishedReg": "1971-03-01", 
        "description": "The variation of silica activity with temperature and pressure for a variety of silica buffers (mineral pairs) allows Ptotal to be calculated for a wide range of igneous rocks. The method also depends on evaluating (\u2202 log aSiO2/\u2202P)T and (\u0394 log aSiO2/\u0394T)p; the former is equivalent to the partial molar volume of silica in silicate liquids, while the latter is estimated from published experiments on natural melts. Results for calc-alkaline rhyolites with phenocrysts of quartz, olivine or orthopyroxene, and iron-titanium oxides, range from 3.45 to 9.58 kilobars; a pantellerite is intermediate at 7.53 kilobars. At 1327\u00b0 C, the silicate inclusions in diamond equilibrated at 63.5 kilobars, and the kimberlite crystallisation path intersected the baddeleyite-zircon reaction at 55.7 kilobars. Two trachybasalts would equilibrate with their lherzolite xenoliths at 17.0 and 21.0 kilobars at surface quenching temperatures. Potassic lavas such as orendites and ugandites at 1300\u00b0 C would be in equilibrium with mantle olivine-orthropyroxene at 35.1 and 69.0 kilobars respectively. Basalts and basaltic-andesites could equilibrate (at 1100\u00b0 C) with quartz at between 24.9 and 26.8 kilobars; quartz can therefore be considered a possible high pressure \u201cxenocryst\u201d in lavas with low Sr87/Sr86 ratios. Andesites will equilibrate at 1300\u00b0 C with the mantle at a depth of 75 kilometres; at greater depths andesite will have a basaltic precursor. In general, lavas with low silica activity will equilibrate at greater depths in the mantle than those with higher silica activities. The Apollo 11 basalts contain minerals which suggest equilibration at 37 kilobars; the calculated quenching temperature is 1009\u00b0 C, from which logfO2 can be derived (\u221215.2) which in turn indicates approximately 0.10% Fe2O3 in these lavas.", 
        "genre": "research_article", 
        "id": "sg:pub.10.1007/bf00373791", 
        "inLanguage": [
          "en"
        ], 
        "isAccessibleForFree": false, 
        "isPartOf": [
          {
            "id": "sg:journal.1026106", 
            "issn": [
              "0010-7999", 
              "1432-0967"
            ], 
            "name": "Contributions to Mineralogy and Petrology", 
            "type": "Periodical"
          }, 
          {
            "issueNumber": "1", 
            "type": "PublicationIssue"
          }, 
          {
            "type": "PublicationVolume", 
            "volumeNumber": "33"
          }
        ], 
        "name": "Silica activity and Ptotal in igneous rocks", 
        "pagination": "1-20", 
        "productId": [
          {
            "name": "doi", 
            "type": "PropertyValue", 
            "value": [
              "10.1007/bf00373791"
            ]
          }, 
          {
            "name": "readcube_id", 
            "type": "PropertyValue", 
            "value": [
              "75845aede3b6c166fa21657762368069d887fb82af2e1050b6f0b1e26461d99e"
            ]
          }, 
          {
            "name": "dimensions_id", 
            "type": "PropertyValue", 
            "value": [
              "pub.1024667496"
            ]
          }
        ], 
        "sameAs": [
          "https://doi.org/10.1007/bf00373791", 
          "https://app.dimensions.ai/details/publication/pub.1024667496"
        ], 
        "sdDataset": "articles", 
        "sdDatePublished": "2019-04-15T08:50", 
        "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_119732_00000000.jsonl", 
        "type": "ScholarlyArticle", 
        "url": "http://link.springer.com/10.1007/BF00373791"
      }
    ]
     

    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/bf00373791'

    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/bf00373791'

    Turtle is a human-readable linked data format.

    curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/bf00373791'

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

    curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/bf00373791'


     

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

    176 TRIPLES      21 PREDICATES      56 URIs      19 LITERALS      7 BLANK NODES

    Subject Predicate Object
    1 sg:pub.10.1007/bf00373791 schema:about anzsrc-for:04
    2 anzsrc-for:0403
    3 schema:author Nd73da446f44a4140bfb7a833f7616039
    4 schema:citation sg:pub.10.1007/bf00370985
    5 sg:pub.10.1007/bf00371806
    6 sg:pub.10.1007/bf00372052
    7 sg:pub.10.1007/bf00386111
    8 sg:pub.10.1007/bf00390081
    9 sg:pub.10.1007/bf00508912
    10 sg:pub.10.1007/bf00518082
    11 sg:pub.10.1007/bf01167214
    12 https://doi.org/10.1002/gj.3350040105
    13 https://doi.org/10.1016/0016-7037(71)90081-0
    14 https://doi.org/10.1016/0031-9201(70)90063-4
    15 https://doi.org/10.1017/s0080456800004798
    16 https://doi.org/10.1029/jb073i006p02261
    17 https://doi.org/10.1029/jb074i022p05301
    18 https://doi.org/10.1029/jb075i032p06480
    19 https://doi.org/10.1029/jz069i020p04377
    20 https://doi.org/10.1086/626745
    21 https://doi.org/10.1093/petrology/3.1.82
    22 https://doi.org/10.1093/petrology/5.2.310
    23 https://doi.org/10.1093/petrology/5.3.435
    24 https://doi.org/10.1098/rsta.1972.0008
    25 https://doi.org/10.1130/0016-7606(1970)81[17:tvacot]2.0.co;2
    26 https://doi.org/10.1130/0016-7606(1970)81[311:sroqlo]2.0.co;2
    27 https://doi.org/10.1130/0016-7606(1970)81[39:srotts]2.0.co;2
    28 https://doi.org/10.1130/spe132-p1
    29 https://doi.org/10.2113/gsecongeo.63.5.495
    30 https://doi.org/10.2475/ajs.269.2.132
    31 https://doi.org/10.2475/ajs.269.2.169
    32 https://doi.org/10.2475/ajs.270.5.334
    33 schema:datePublished 1971-03
    34 schema:datePublishedReg 1971-03-01
    35 schema:description The variation of silica activity with temperature and pressure for a variety of silica buffers (mineral pairs) allows Ptotal to be calculated for a wide range of igneous rocks. The method also depends on evaluating (∂ log aSiO2/∂P)T and (Δ log aSiO2/ΔT)p; the former is equivalent to the partial molar volume of silica in silicate liquids, while the latter is estimated from published experiments on natural melts. Results for calc-alkaline rhyolites with phenocrysts of quartz, olivine or orthopyroxene, and iron-titanium oxides, range from 3.45 to 9.58 kilobars; a pantellerite is intermediate at 7.53 kilobars. At 1327° C, the silicate inclusions in diamond equilibrated at 63.5 kilobars, and the kimberlite crystallisation path intersected the baddeleyite-zircon reaction at 55.7 kilobars. Two trachybasalts would equilibrate with their lherzolite xenoliths at 17.0 and 21.0 kilobars at surface quenching temperatures. Potassic lavas such as orendites and ugandites at 1300° C would be in equilibrium with mantle olivine-orthropyroxene at 35.1 and 69.0 kilobars respectively. Basalts and basaltic-andesites could equilibrate (at 1100° C) with quartz at between 24.9 and 26.8 kilobars; quartz can therefore be considered a possible high pressure “xenocryst” in lavas with low Sr87/Sr86 ratios. Andesites will equilibrate at 1300° C with the mantle at a depth of 75 kilometres; at greater depths andesite will have a basaltic precursor. In general, lavas with low silica activity will equilibrate at greater depths in the mantle than those with higher silica activities. The Apollo 11 basalts contain minerals which suggest equilibration at 37 kilobars; the calculated quenching temperature is 1009° C, from which logfO2 can be derived (−15.2) which in turn indicates approximately 0.10% Fe2O3 in these lavas.
    36 schema:genre research_article
    37 schema:inLanguage en
    38 schema:isAccessibleForFree false
    39 schema:isPartOf N6166c8a8c841491a9b10c9ef402a4e7e
    40 N6c91e03897df48c4a590bfb6bdc8d791
    41 sg:journal.1026106
    42 schema:name Silica activity and Ptotal in igneous rocks
    43 schema:pagination 1-20
    44 schema:productId N108e8c0b15324deb813342a893580235
    45 N5ba38f2819ee45b592565baa221537ea
    46 Na45ef42cf4f4493ba5766c420afda14f
    47 schema:sameAs https://app.dimensions.ai/details/publication/pub.1024667496
    48 https://doi.org/10.1007/bf00373791
    49 schema:sdDatePublished 2019-04-15T08:50
    50 schema:sdLicense https://scigraph.springernature.com/explorer/license/
    51 schema:sdPublisher N50ba1dcab9734aaeb76f2eed4e963fb1
    52 schema:url http://link.springer.com/10.1007/BF00373791
    53 sgo:license sg:explorer/license/
    54 sgo:sdDataset articles
    55 rdf:type schema:ScholarlyArticle
    56 N108e8c0b15324deb813342a893580235 schema:name dimensions_id
    57 schema:value pub.1024667496
    58 rdf:type schema:PropertyValue
    59 N3f826c5ca7dd40d9831c5d9ff9cbcc51 rdf:first sg:person.01157747754.50
    60 rdf:rest N483e7e2528484a60842a5df3cb44e315
    61 N483e7e2528484a60842a5df3cb44e315 rdf:first sg:person.01251612234.88
    62 rdf:rest rdf:nil
    63 N50ba1dcab9734aaeb76f2eed4e963fb1 schema:name Springer Nature - SN SciGraph project
    64 rdf:type schema:Organization
    65 N5ba38f2819ee45b592565baa221537ea schema:name readcube_id
    66 schema:value 75845aede3b6c166fa21657762368069d887fb82af2e1050b6f0b1e26461d99e
    67 rdf:type schema:PropertyValue
    68 N6166c8a8c841491a9b10c9ef402a4e7e schema:issueNumber 1
    69 rdf:type schema:PublicationIssue
    70 N6c91e03897df48c4a590bfb6bdc8d791 schema:volumeNumber 33
    71 rdf:type schema:PublicationVolume
    72 Na45ef42cf4f4493ba5766c420afda14f schema:name doi
    73 schema:value 10.1007/bf00373791
    74 rdf:type schema:PropertyValue
    75 Nd73da446f44a4140bfb7a833f7616039 rdf:first sg:person.016604357276.36
    76 rdf:rest N3f826c5ca7dd40d9831c5d9ff9cbcc51
    77 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
    78 schema:name Earth Sciences
    79 rdf:type schema:DefinedTerm
    80 anzsrc-for:0403 schema:inDefinedTermSet anzsrc-for:
    81 schema:name Geology
    82 rdf:type schema:DefinedTerm
    83 sg:journal.1026106 schema:issn 0010-7999
    84 1432-0967
    85 schema:name Contributions to Mineralogy and Petrology
    86 rdf:type schema:Periodical
    87 sg:person.01157747754.50 schema:affiliation https://www.grid.ac/institutes/grid.47840.3f
    88 schema:familyName Carmichael
    89 schema:givenName I. S. E.
    90 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.01157747754.50
    91 rdf:type schema:Person
    92 sg:person.01251612234.88 schema:affiliation https://www.grid.ac/institutes/grid.213876.9
    93 schema:familyName Stormer
    94 schema:givenName J. C.
    95 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.01251612234.88
    96 rdf:type schema:Person
    97 sg:person.016604357276.36 schema:affiliation https://www.grid.ac/institutes/grid.22072.35
    98 schema:familyName Nicholls
    99 schema:givenName J.
    100 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.016604357276.36
    101 rdf:type schema:Person
    102 sg:pub.10.1007/bf00370985 schema:sameAs https://app.dimensions.ai/details/publication/pub.1022578692
    103 https://doi.org/10.1007/bf00370985
    104 rdf:type schema:CreativeWork
    105 sg:pub.10.1007/bf00371806 schema:sameAs https://app.dimensions.ai/details/publication/pub.1028685359
    106 https://doi.org/10.1007/bf00371806
    107 rdf:type schema:CreativeWork
    108 sg:pub.10.1007/bf00372052 schema:sameAs https://app.dimensions.ai/details/publication/pub.1039651157
    109 https://doi.org/10.1007/bf00372052
    110 rdf:type schema:CreativeWork
    111 sg:pub.10.1007/bf00386111 schema:sameAs https://app.dimensions.ai/details/publication/pub.1048833295
    112 https://doi.org/10.1007/bf00386111
    113 rdf:type schema:CreativeWork
    114 sg:pub.10.1007/bf00390081 schema:sameAs https://app.dimensions.ai/details/publication/pub.1019967277
    115 https://doi.org/10.1007/bf00390081
    116 rdf:type schema:CreativeWork
    117 sg:pub.10.1007/bf00508912 schema:sameAs https://app.dimensions.ai/details/publication/pub.1039435514
    118 https://doi.org/10.1007/bf00508912
    119 rdf:type schema:CreativeWork
    120 sg:pub.10.1007/bf00518082 schema:sameAs https://app.dimensions.ai/details/publication/pub.1025265667
    121 https://doi.org/10.1007/bf00518082
    122 rdf:type schema:CreativeWork
    123 sg:pub.10.1007/bf01167214 schema:sameAs https://app.dimensions.ai/details/publication/pub.1020017210
    124 https://doi.org/10.1007/bf01167214
    125 rdf:type schema:CreativeWork
    126 https://doi.org/10.1002/gj.3350040105 schema:sameAs https://app.dimensions.ai/details/publication/pub.1010189291
    127 rdf:type schema:CreativeWork
    128 https://doi.org/10.1016/0016-7037(71)90081-0 schema:sameAs https://app.dimensions.ai/details/publication/pub.1047227336
    129 rdf:type schema:CreativeWork
    130 https://doi.org/10.1016/0031-9201(70)90063-4 schema:sameAs https://app.dimensions.ai/details/publication/pub.1007052186
    131 rdf:type schema:CreativeWork
    132 https://doi.org/10.1017/s0080456800004798 schema:sameAs https://app.dimensions.ai/details/publication/pub.1010467576
    133 rdf:type schema:CreativeWork
    134 https://doi.org/10.1029/jb073i006p02261 schema:sameAs https://app.dimensions.ai/details/publication/pub.1010859157
    135 rdf:type schema:CreativeWork
    136 https://doi.org/10.1029/jb074i022p05301 schema:sameAs https://app.dimensions.ai/details/publication/pub.1017380337
    137 rdf:type schema:CreativeWork
    138 https://doi.org/10.1029/jb075i032p06480 schema:sameAs https://app.dimensions.ai/details/publication/pub.1050239594
    139 rdf:type schema:CreativeWork
    140 https://doi.org/10.1029/jz069i020p04377 schema:sameAs https://app.dimensions.ai/details/publication/pub.1019241559
    141 rdf:type schema:CreativeWork
    142 https://doi.org/10.1086/626745 schema:sameAs https://app.dimensions.ai/details/publication/pub.1058822527
    143 rdf:type schema:CreativeWork
    144 https://doi.org/10.1093/petrology/3.1.82 schema:sameAs https://app.dimensions.ai/details/publication/pub.1059972823
    145 rdf:type schema:CreativeWork
    146 https://doi.org/10.1093/petrology/5.2.310 schema:sameAs https://app.dimensions.ai/details/publication/pub.1059973282
    147 rdf:type schema:CreativeWork
    148 https://doi.org/10.1093/petrology/5.3.435 schema:sameAs https://app.dimensions.ai/details/publication/pub.1059973285
    149 rdf:type schema:CreativeWork
    150 https://doi.org/10.1098/rsta.1972.0008 schema:sameAs https://app.dimensions.ai/details/publication/pub.1011930216
    151 rdf:type schema:CreativeWork
    152 https://doi.org/10.1130/0016-7606(1970)81[17:tvacot]2.0.co;2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1026021765
    153 rdf:type schema:CreativeWork
    154 https://doi.org/10.1130/0016-7606(1970)81[311:sroqlo]2.0.co;2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1014383871
    155 rdf:type schema:CreativeWork
    156 https://doi.org/10.1130/0016-7606(1970)81[39:srotts]2.0.co;2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1039472297
    157 rdf:type schema:CreativeWork
    158 https://doi.org/10.1130/spe132-p1 schema:sameAs https://app.dimensions.ai/details/publication/pub.1088804973
    159 rdf:type schema:CreativeWork
    160 https://doi.org/10.2113/gsecongeo.63.5.495 schema:sameAs https://app.dimensions.ai/details/publication/pub.1068929885
    161 rdf:type schema:CreativeWork
    162 https://doi.org/10.2475/ajs.269.2.132 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070840859
    163 rdf:type schema:CreativeWork
    164 https://doi.org/10.2475/ajs.269.2.169 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070840860
    165 rdf:type schema:CreativeWork
    166 https://doi.org/10.2475/ajs.270.5.334 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070840915
    167 rdf:type schema:CreativeWork
    168 https://www.grid.ac/institutes/grid.213876.9 schema:alternateName University of Georgia
    169 schema:name Dept. of Geology, University of Georgia, 30601, Athens, Georgia
    170 rdf:type schema:Organization
    171 https://www.grid.ac/institutes/grid.22072.35 schema:alternateName University of Calgary
    172 schema:name Dept. of Geology, University of Calgary, Alberta, Canada
    173 rdf:type schema:Organization
    174 https://www.grid.ac/institutes/grid.47840.3f schema:alternateName University of California, Berkeley
    175 schema:name Dept. of Geology and Geophysics, University of California, 94720, Berkeley, Calif.
    176 rdf:type schema:Organization
     




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


    ...