Metamorphism in oceanic layer 3, Gorringe Bank, eastern Atlantic View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1988-12

AUTHORS

Catherine Mevel

ABSTRACT

Gorringe Bank is an anomalously high structure of the eastern part of the north Atlantic, which was known to be composed of mantle-derived peridotites (layer 4) and gabbros (layer 3). During the submersible cruise CYAGOR II in 1981, the contact between layer 4 and layer 3 was observed on Mount Gettysburg and interpreted as tectonic. The overlying series of gabbro was extensively sampled on both mounts composing the bank, Gettysburg and Ormonde. Coarse-grained to pegmatoid clinopyroxene gabbros predominate and are associated with differentiated rocks (ferrogabbros and diorites). Cumulate gabbros are missing. The gabbroic section sampled is therefore interpreted as the upper part of the plutonic section. Most samples were strongly recrystallized during two distinct events. Metamorphism occurred close to the ridge axis, from interaction of a seawater-derived fluid with still hot gabbros. High temperature shear zones favoured fluid circulation, but the water/rock ratio — estimated from the sodium input — was very small in undeformed rocks (<1). The low W/R ratio explains the strong evolution of the fluid phase and therefore some particular compositions of secondary minerals. Low temperature alteration occurred when the gabbros were tectonically emplaced close to the sea bottom. More... »

PAGES

496-509

Journal

Author Affiliations

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/bf00371379

DOI

http://dx.doi.org/10.1007/bf00371379

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1026063181


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": "Sorbonne University", 
          "id": "https://www.grid.ac/institutes/grid.462844.8", 
          "name": [
            "Laboratoire de p\u00e9trologie M\u00e9tamorphique, UA 727, Universit\u00e9 Pierre et Marie Curie, 4 place Jussieu, F-75252, Paris cedex, France"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Mevel", 
        "givenName": "Catherine", 
        "id": "sg:person.011757207573.37", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.011757207573.37"
        ], 
        "type": "Person"
      }
    ], 
    "citation": [
      {
        "id": "sg:pub.10.1007/bf00371544", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001173133", 
          "https://doi.org/10.1007/bf00371544"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00371544", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001173133", 
          "https://doi.org/10.1007/bf00371544"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/jb092ib09p09175", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001353977"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(83)90276-4", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001514155"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(83)90276-4", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001514155"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(83)90193-0", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001745047"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(83)90193-0", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001745047"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(86)90184-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1002199129"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1038/275211a0", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1003814825", 
          "https://doi.org/10.1038/275211a0"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(86)90042-7", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1011039697"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(86)90042-7", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1011039697"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0191-8141(83)90027-5", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1012978133"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0191-8141(83)90027-5", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1012978133"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(85)90177-3", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1015927234"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(85)90177-3", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1015927234"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/tc004i004p00395", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1017850497"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00399714", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1018927968", 
          "https://doi.org/10.1007/bf00399714"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00399714", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1018927968", 
          "https://doi.org/10.1007/bf00399714"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(82)90048-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1022118078"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(82)90048-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1022118078"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(85)90189-9", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1024934087"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(85)90189-9", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1024934087"
        ], 
        "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": "https://doi.org/10.1016/0012-821x(78)90146-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1025612543"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(78)90146-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1025612543"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00376960", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1026047628", 
          "https://doi.org/10.1007/bf00376960"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00376960", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1026047628", 
          "https://doi.org/10.1007/bf00376960"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(87)90050-1", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1026615010"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(87)90050-1", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1026615010"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(79)90174-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1027844389"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(79)90174-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1027844389"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2113/gssgfbull.s7-xxi.5.557", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1029787465"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(82)90186-8", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1029992525"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(82)90186-8", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1029992525"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(87)90051-3", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1031459953"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(87)90051-3", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1031459953"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/jb086ib04p02737", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1032853651"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(81)90186-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1034126334"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(81)90186-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1034126334"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0025-3227(82)90022-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1037006969"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0025-3227(82)90022-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1037006969"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1139/e77-083", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1040249471"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(78)90107-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1041052742"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(78)90107-2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1041052742"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(84)90169-9", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1043737286"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(84)90169-9", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1043737286"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1144/gsl.sp.1984.013.01.10", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1045015663"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/jb089ib13p11379", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1046353447"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/gl006i011p00829", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1046852167"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1130/0016-7606(1983)94<161:mahsat>2.0.co;2", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1049473320"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(85)90222-4", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1052751269"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0016-7037(85)90222-4", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1052751269"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/jb081i023p04135", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1052930954"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/jb089ib05p03275", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1053358769"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0009-2541(67)90004-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1053518089"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0009-2541(67)90004-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1053518089"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1086/628045", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1058823827"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1086/628635", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1058824417"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1093/petrology/13.1.99", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1059972300"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1093/petrology/18.1.53", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1059972422"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2475/ajs.274.6.613", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1070841158"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2475/ajs.281.6.697", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1070841627"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2475/ajs.283.1.48", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1070841722"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2973/dsdp.proc.13.1973", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1099217963"
        ], 
        "type": "CreativeWork"
      }
    ], 
    "datePublished": "1988-12", 
    "datePublishedReg": "1988-12-01", 
    "description": "Gorringe Bank is an anomalously high structure of the eastern part of the north Atlantic, which was known to be composed of mantle-derived peridotites (layer 4) and gabbros (layer 3). During the submersible cruise CYAGOR II in 1981, the contact between layer 4 and layer 3 was observed on Mount Gettysburg and interpreted as tectonic. The overlying series of gabbro was extensively sampled on both mounts composing the bank, Gettysburg and Ormonde. Coarse-grained to pegmatoid clinopyroxene gabbros predominate and are associated with differentiated rocks (ferrogabbros and diorites). Cumulate gabbros are missing. The gabbroic section sampled is therefore interpreted as the upper part of the plutonic section. Most samples were strongly recrystallized during two distinct events. Metamorphism occurred close to the ridge axis, from interaction of a seawater-derived fluid with still hot gabbros. High temperature shear zones favoured fluid circulation, but the water/rock ratio \u2014 estimated from the sodium input \u2014 was very small in undeformed rocks (<1). The low W/R ratio explains the strong evolution of the fluid phase and therefore some particular compositions of secondary minerals. Low temperature alteration occurred when the gabbros were tectonically emplaced close to the sea bottom.", 
    "genre": "research_article", 
    "id": "sg:pub.10.1007/bf00371379", 
    "inLanguage": [
      "en"
    ], 
    "isAccessibleForFree": false, 
    "isPartOf": [
      {
        "id": "sg:journal.1026106", 
        "issn": [
          "0010-7999", 
          "1432-0967"
        ], 
        "name": "Contributions to Mineralogy and Petrology", 
        "type": "Periodical"
      }, 
      {
        "issueNumber": "4", 
        "type": "PublicationIssue"
      }, 
      {
        "type": "PublicationVolume", 
        "volumeNumber": "100"
      }
    ], 
    "name": "Metamorphism in oceanic layer 3, Gorringe Bank, eastern Atlantic", 
    "pagination": "496-509", 
    "productId": [
      {
        "name": "doi", 
        "type": "PropertyValue", 
        "value": [
          "10.1007/bf00371379"
        ]
      }, 
      {
        "name": "readcube_id", 
        "type": "PropertyValue", 
        "value": [
          "7c29eb913d558c264c0470f45b8140907990e4e25edfcbfb91bc14467d9ebcb0"
        ]
      }, 
      {
        "name": "dimensions_id", 
        "type": "PropertyValue", 
        "value": [
          "pub.1026063181"
        ]
      }
    ], 
    "sameAs": [
      "https://doi.org/10.1007/bf00371379", 
      "https://app.dimensions.ai/details/publication/pub.1026063181"
    ], 
    "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_119724_00000000.jsonl", 
    "type": "ScholarlyArticle", 
    "url": "http://link.springer.com/10.1007/BF00371379"
  }
]
 

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/bf00371379'

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/bf00371379'

Turtle is a human-readable linked data format.

curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/bf00371379'

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

curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/bf00371379'


 

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

195 TRIPLES      21 PREDICATES      70 URIs      19 LITERALS      7 BLANK NODES

Subject Predicate Object
1 sg:pub.10.1007/bf00371379 schema:about anzsrc-for:04
2 anzsrc-for:0403
3 schema:author N53ec7494437e4adf8b3856a657d51bdd
4 schema:citation sg:pub.10.1007/bf00371544
5 sg:pub.10.1007/bf00376960
6 sg:pub.10.1007/bf00383440
7 sg:pub.10.1007/bf00399714
8 sg:pub.10.1038/275211a0
9 https://doi.org/10.1016/0009-2541(67)90004-6
10 https://doi.org/10.1016/0012-821x(78)90146-2
11 https://doi.org/10.1016/0012-821x(79)90174-2
12 https://doi.org/10.1016/0012-821x(81)90186-2
13 https://doi.org/10.1016/0012-821x(82)90048-6
14 https://doi.org/10.1016/0012-821x(82)90186-8
15 https://doi.org/10.1016/0012-821x(83)90193-0
16 https://doi.org/10.1016/0012-821x(84)90169-9
17 https://doi.org/10.1016/0012-821x(85)90177-3
18 https://doi.org/10.1016/0012-821x(86)90042-7
19 https://doi.org/10.1016/0012-821x(86)90184-6
20 https://doi.org/10.1016/0012-821x(87)90050-1
21 https://doi.org/10.1016/0012-821x(87)90051-3
22 https://doi.org/10.1016/0016-7037(78)90107-2
23 https://doi.org/10.1016/0016-7037(83)90276-4
24 https://doi.org/10.1016/0016-7037(85)90189-9
25 https://doi.org/10.1016/0016-7037(85)90222-4
26 https://doi.org/10.1016/0025-3227(82)90022-6
27 https://doi.org/10.1016/0191-8141(83)90027-5
28 https://doi.org/10.1029/gl006i011p00829
29 https://doi.org/10.1029/jb081i023p04135
30 https://doi.org/10.1029/jb086ib04p02737
31 https://doi.org/10.1029/jb089ib05p03275
32 https://doi.org/10.1029/jb089ib13p11379
33 https://doi.org/10.1029/jb092ib09p09175
34 https://doi.org/10.1029/tc004i004p00395
35 https://doi.org/10.1086/628045
36 https://doi.org/10.1086/628635
37 https://doi.org/10.1093/petrology/13.1.99
38 https://doi.org/10.1093/petrology/18.1.53
39 https://doi.org/10.1130/0016-7606(1983)94<161:mahsat>2.0.co;2
40 https://doi.org/10.1139/e77-083
41 https://doi.org/10.1144/gsl.sp.1984.013.01.10
42 https://doi.org/10.2113/gssgfbull.s7-xxi.5.557
43 https://doi.org/10.2475/ajs.274.6.613
44 https://doi.org/10.2475/ajs.281.6.697
45 https://doi.org/10.2475/ajs.283.1.48
46 https://doi.org/10.2973/dsdp.proc.13.1973
47 schema:datePublished 1988-12
48 schema:datePublishedReg 1988-12-01
49 schema:description Gorringe Bank is an anomalously high structure of the eastern part of the north Atlantic, which was known to be composed of mantle-derived peridotites (layer 4) and gabbros (layer 3). During the submersible cruise CYAGOR II in 1981, the contact between layer 4 and layer 3 was observed on Mount Gettysburg and interpreted as tectonic. The overlying series of gabbro was extensively sampled on both mounts composing the bank, Gettysburg and Ormonde. Coarse-grained to pegmatoid clinopyroxene gabbros predominate and are associated with differentiated rocks (ferrogabbros and diorites). Cumulate gabbros are missing. The gabbroic section sampled is therefore interpreted as the upper part of the plutonic section. Most samples were strongly recrystallized during two distinct events. Metamorphism occurred close to the ridge axis, from interaction of a seawater-derived fluid with still hot gabbros. High temperature shear zones favoured fluid circulation, but the water/rock ratio — estimated from the sodium input — was very small in undeformed rocks (<1). The low W/R ratio explains the strong evolution of the fluid phase and therefore some particular compositions of secondary minerals. Low temperature alteration occurred when the gabbros were tectonically emplaced close to the sea bottom.
50 schema:genre research_article
51 schema:inLanguage en
52 schema:isAccessibleForFree false
53 schema:isPartOf N43de7598c3e34a4eab40523ae45c27eb
54 N5ac594435d85489e82b3b6a9dabdd4e3
55 sg:journal.1026106
56 schema:name Metamorphism in oceanic layer 3, Gorringe Bank, eastern Atlantic
57 schema:pagination 496-509
58 schema:productId N10dd67bf17e64326bce7a04faff7763c
59 Nbf8502c4555a4712919eefe1cf567276
60 Nc85e4cc729cb4ceab857a998c40b31e6
61 schema:sameAs https://app.dimensions.ai/details/publication/pub.1026063181
62 https://doi.org/10.1007/bf00371379
63 schema:sdDatePublished 2019-04-15T08:49
64 schema:sdLicense https://scigraph.springernature.com/explorer/license/
65 schema:sdPublisher Nf0dac17fca7c453eb4c3d1693b6bd4bf
66 schema:url http://link.springer.com/10.1007/BF00371379
67 sgo:license sg:explorer/license/
68 sgo:sdDataset articles
69 rdf:type schema:ScholarlyArticle
70 N10dd67bf17e64326bce7a04faff7763c schema:name doi
71 schema:value 10.1007/bf00371379
72 rdf:type schema:PropertyValue
73 N43de7598c3e34a4eab40523ae45c27eb schema:volumeNumber 100
74 rdf:type schema:PublicationVolume
75 N53ec7494437e4adf8b3856a657d51bdd rdf:first sg:person.011757207573.37
76 rdf:rest rdf:nil
77 N5ac594435d85489e82b3b6a9dabdd4e3 schema:issueNumber 4
78 rdf:type schema:PublicationIssue
79 Nbf8502c4555a4712919eefe1cf567276 schema:name dimensions_id
80 schema:value pub.1026063181
81 rdf:type schema:PropertyValue
82 Nc85e4cc729cb4ceab857a998c40b31e6 schema:name readcube_id
83 schema:value 7c29eb913d558c264c0470f45b8140907990e4e25edfcbfb91bc14467d9ebcb0
84 rdf:type schema:PropertyValue
85 Nf0dac17fca7c453eb4c3d1693b6bd4bf schema:name Springer Nature - SN SciGraph project
86 rdf:type schema:Organization
87 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
88 schema:name Earth Sciences
89 rdf:type schema:DefinedTerm
90 anzsrc-for:0403 schema:inDefinedTermSet anzsrc-for:
91 schema:name Geology
92 rdf:type schema:DefinedTerm
93 sg:journal.1026106 schema:issn 0010-7999
94 1432-0967
95 schema:name Contributions to Mineralogy and Petrology
96 rdf:type schema:Periodical
97 sg:person.011757207573.37 schema:affiliation https://www.grid.ac/institutes/grid.462844.8
98 schema:familyName Mevel
99 schema:givenName Catherine
100 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.011757207573.37
101 rdf:type schema:Person
102 sg:pub.10.1007/bf00371544 schema:sameAs https://app.dimensions.ai/details/publication/pub.1001173133
103 https://doi.org/10.1007/bf00371544
104 rdf:type schema:CreativeWork
105 sg:pub.10.1007/bf00376960 schema:sameAs https://app.dimensions.ai/details/publication/pub.1026047628
106 https://doi.org/10.1007/bf00376960
107 rdf:type schema:CreativeWork
108 sg:pub.10.1007/bf00383440 schema:sameAs https://app.dimensions.ai/details/publication/pub.1024979251
109 https://doi.org/10.1007/bf00383440
110 rdf:type schema:CreativeWork
111 sg:pub.10.1007/bf00399714 schema:sameAs https://app.dimensions.ai/details/publication/pub.1018927968
112 https://doi.org/10.1007/bf00399714
113 rdf:type schema:CreativeWork
114 sg:pub.10.1038/275211a0 schema:sameAs https://app.dimensions.ai/details/publication/pub.1003814825
115 https://doi.org/10.1038/275211a0
116 rdf:type schema:CreativeWork
117 https://doi.org/10.1016/0009-2541(67)90004-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1053518089
118 rdf:type schema:CreativeWork
119 https://doi.org/10.1016/0012-821x(78)90146-2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1025612543
120 rdf:type schema:CreativeWork
121 https://doi.org/10.1016/0012-821x(79)90174-2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1027844389
122 rdf:type schema:CreativeWork
123 https://doi.org/10.1016/0012-821x(81)90186-2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1034126334
124 rdf:type schema:CreativeWork
125 https://doi.org/10.1016/0012-821x(82)90048-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1022118078
126 rdf:type schema:CreativeWork
127 https://doi.org/10.1016/0012-821x(82)90186-8 schema:sameAs https://app.dimensions.ai/details/publication/pub.1029992525
128 rdf:type schema:CreativeWork
129 https://doi.org/10.1016/0012-821x(83)90193-0 schema:sameAs https://app.dimensions.ai/details/publication/pub.1001745047
130 rdf:type schema:CreativeWork
131 https://doi.org/10.1016/0012-821x(84)90169-9 schema:sameAs https://app.dimensions.ai/details/publication/pub.1043737286
132 rdf:type schema:CreativeWork
133 https://doi.org/10.1016/0012-821x(85)90177-3 schema:sameAs https://app.dimensions.ai/details/publication/pub.1015927234
134 rdf:type schema:CreativeWork
135 https://doi.org/10.1016/0012-821x(86)90042-7 schema:sameAs https://app.dimensions.ai/details/publication/pub.1011039697
136 rdf:type schema:CreativeWork
137 https://doi.org/10.1016/0012-821x(86)90184-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1002199129
138 rdf:type schema:CreativeWork
139 https://doi.org/10.1016/0012-821x(87)90050-1 schema:sameAs https://app.dimensions.ai/details/publication/pub.1026615010
140 rdf:type schema:CreativeWork
141 https://doi.org/10.1016/0012-821x(87)90051-3 schema:sameAs https://app.dimensions.ai/details/publication/pub.1031459953
142 rdf:type schema:CreativeWork
143 https://doi.org/10.1016/0016-7037(78)90107-2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041052742
144 rdf:type schema:CreativeWork
145 https://doi.org/10.1016/0016-7037(83)90276-4 schema:sameAs https://app.dimensions.ai/details/publication/pub.1001514155
146 rdf:type schema:CreativeWork
147 https://doi.org/10.1016/0016-7037(85)90189-9 schema:sameAs https://app.dimensions.ai/details/publication/pub.1024934087
148 rdf:type schema:CreativeWork
149 https://doi.org/10.1016/0016-7037(85)90222-4 schema:sameAs https://app.dimensions.ai/details/publication/pub.1052751269
150 rdf:type schema:CreativeWork
151 https://doi.org/10.1016/0025-3227(82)90022-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1037006969
152 rdf:type schema:CreativeWork
153 https://doi.org/10.1016/0191-8141(83)90027-5 schema:sameAs https://app.dimensions.ai/details/publication/pub.1012978133
154 rdf:type schema:CreativeWork
155 https://doi.org/10.1029/gl006i011p00829 schema:sameAs https://app.dimensions.ai/details/publication/pub.1046852167
156 rdf:type schema:CreativeWork
157 https://doi.org/10.1029/jb081i023p04135 schema:sameAs https://app.dimensions.ai/details/publication/pub.1052930954
158 rdf:type schema:CreativeWork
159 https://doi.org/10.1029/jb086ib04p02737 schema:sameAs https://app.dimensions.ai/details/publication/pub.1032853651
160 rdf:type schema:CreativeWork
161 https://doi.org/10.1029/jb089ib05p03275 schema:sameAs https://app.dimensions.ai/details/publication/pub.1053358769
162 rdf:type schema:CreativeWork
163 https://doi.org/10.1029/jb089ib13p11379 schema:sameAs https://app.dimensions.ai/details/publication/pub.1046353447
164 rdf:type schema:CreativeWork
165 https://doi.org/10.1029/jb092ib09p09175 schema:sameAs https://app.dimensions.ai/details/publication/pub.1001353977
166 rdf:type schema:CreativeWork
167 https://doi.org/10.1029/tc004i004p00395 schema:sameAs https://app.dimensions.ai/details/publication/pub.1017850497
168 rdf:type schema:CreativeWork
169 https://doi.org/10.1086/628045 schema:sameAs https://app.dimensions.ai/details/publication/pub.1058823827
170 rdf:type schema:CreativeWork
171 https://doi.org/10.1086/628635 schema:sameAs https://app.dimensions.ai/details/publication/pub.1058824417
172 rdf:type schema:CreativeWork
173 https://doi.org/10.1093/petrology/13.1.99 schema:sameAs https://app.dimensions.ai/details/publication/pub.1059972300
174 rdf:type schema:CreativeWork
175 https://doi.org/10.1093/petrology/18.1.53 schema:sameAs https://app.dimensions.ai/details/publication/pub.1059972422
176 rdf:type schema:CreativeWork
177 https://doi.org/10.1130/0016-7606(1983)94<161:mahsat>2.0.co;2 schema:sameAs https://app.dimensions.ai/details/publication/pub.1049473320
178 rdf:type schema:CreativeWork
179 https://doi.org/10.1139/e77-083 schema:sameAs https://app.dimensions.ai/details/publication/pub.1040249471
180 rdf:type schema:CreativeWork
181 https://doi.org/10.1144/gsl.sp.1984.013.01.10 schema:sameAs https://app.dimensions.ai/details/publication/pub.1045015663
182 rdf:type schema:CreativeWork
183 https://doi.org/10.2113/gssgfbull.s7-xxi.5.557 schema:sameAs https://app.dimensions.ai/details/publication/pub.1029787465
184 rdf:type schema:CreativeWork
185 https://doi.org/10.2475/ajs.274.6.613 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070841158
186 rdf:type schema:CreativeWork
187 https://doi.org/10.2475/ajs.281.6.697 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070841627
188 rdf:type schema:CreativeWork
189 https://doi.org/10.2475/ajs.283.1.48 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070841722
190 rdf:type schema:CreativeWork
191 https://doi.org/10.2973/dsdp.proc.13.1973 schema:sameAs https://app.dimensions.ai/details/publication/pub.1099217963
192 rdf:type schema:CreativeWork
193 https://www.grid.ac/institutes/grid.462844.8 schema:alternateName Sorbonne University
194 schema:name Laboratoire de pétrologie Métamorphique, UA 727, Université Pierre et Marie Curie, 4 place Jussieu, F-75252, Paris cedex, France
195 rdf:type schema:Organization
 




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


...