Dépliage 3-D des anticlinaux bordant le synclinal fermé de la vallée des Ponts, Jura central, Suisse View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2004-08

AUTHORS

Benoît Valley, Martin Burkhard, Pierre-André Schnegg

ABSTRACT

The Ponts valley syncline is a closed basin within the Neuchâtel Jura fold and thrust belt. This syncline, apparently uplifted to an altitude of around 1000m is closed in the SW by an anticline with an oblique WNW-ESE direction. The 3-D geometry of the entire structure is examined and unfolded in detail. This syncline is filled with an unexpectedly thick series (~400m) of Tertiairy Molasse, as revealed by the CS-AMT (controlled source audio-magneto-telluric) and a reflexion seismic line. The latter also documents internal compressional structures within the well layered upper freshwater Molasse series. The 3-D configuration of the top Malm limestones has been constructed for the entire area based on new detailed geologic and structural mapping, hundreds of dip measurements, as well as geophysical data. The Malm marker bed displays three distinct types of structures: 1) Thrust faults with shallow dips, vergent to the NW and/or SE that are associated with folds interpreted as fault bend folds; 2) high angle inverse faults, mostly with a SE vergence are interpreted as inverted normal faults, inherited from a modest Oligo-Miocene extensional phase in a NW-SE direction; and 3) tear faults with a dominant N-S direction, probably inherited from an Oligocene extensional phase in association with the opening of the Rhine and Bresse grabens. Tear faults accommodate important lateral changes in fold geometry during the Late Miocene main folding-and-thrusting phase. All deformations are easily explained in an entirely thin-skinned fashion, taking place above a thick detachment horizon within Triassic evaporite series. More... »

PAGES

279-291

Journal

TITLE

Eclogae Geologicae Helvetiae

ISSUE

2

VOLUME

97

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s00015-004-1124-7

DOI

http://dx.doi.org/10.1007/s00015-004-1124-7

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1035838701


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": {
          "name": [
            "Institut de G\u00e9ologie, Rue E.Argand 11, Case Postale, 2007, Neuch\u00e2tel, Switzerland"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Valley", 
        "givenName": "Beno\u00eet", 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "name": [
            "Institut de G\u00e9ologie, Rue E.Argand 11, Case Postale, 2007, Neuch\u00e2tel, Switzerland"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Burkhard", 
        "givenName": "Martin", 
        "id": "sg:person.07717024445.64", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.07717024445.64"
        ], 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "name": [
            "Institut de G\u00e9ologie, Rue E.Argand 11, Case Postale, 2007, Neuch\u00e2tel, Switzerland"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Schnegg", 
        "givenName": "Pierre-Andr\u00e9", 
        "id": "sg:person.0666663007.59", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.0666663007.59"
        ], 
        "type": "Person"
      }
    ], 
    "citation": [
      {
        "id": "https://doi.org/10.1146/annurev.ea.18.050190.000415", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1001712011"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0040-1951(91)90363-w", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1018837617"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0040-1951(91)90363-w", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1018837617"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/s0191-8141(96)00104-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1021579079"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/2002jb002270", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1023483548"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/s0012-821x(99)00238-1", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1030287983"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1144/gsl.sp.1998.134.01.13", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1033272475"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/s0191-8141(99)00021-8", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1040845579"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf02986582", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1044193617", 
          "https://doi.org/10.1007/bf02986582"
        ], 
        "type": "CreativeWork"
      }
    ], 
    "datePublished": "2004-08", 
    "datePublishedReg": "2004-08-01", 
    "description": "The Ponts valley syncline is a closed basin within the Neuch\u00e2tel Jura fold and thrust belt. This syncline, apparently uplifted to an altitude of around 1000m is closed in the SW by an anticline with an oblique WNW-ESE direction. The 3-D geometry of the entire structure is examined and unfolded in detail. This syncline is filled with an unexpectedly thick series (~400m) of Tertiairy Molasse, as revealed by the CS-AMT (controlled source audio-magneto-telluric) and a reflexion seismic line. The latter also documents internal compressional structures within the well layered upper freshwater Molasse series. The 3-D configuration of the top Malm limestones has been constructed for the entire area based on new detailed geologic and structural mapping, hundreds of dip measurements, as well as geophysical data. The Malm marker bed displays three distinct types of structures: 1) Thrust faults with shallow dips, vergent to the NW and/or SE that are associated with folds interpreted as fault bend folds; 2) high angle inverse faults, mostly with a SE vergence are interpreted as inverted normal faults, inherited from a modest Oligo-Miocene extensional phase in a NW-SE direction; and 3) tear faults with a dominant N-S direction, probably inherited from an Oligocene extensional phase in association with the opening of the Rhine and Bresse grabens. Tear faults accommodate important lateral changes in fold geometry during the Late Miocene main folding-and-thrusting phase. All deformations are easily explained in an entirely thin-skinned fashion, taking place above a thick detachment horizon within Triassic evaporite series.", 
    "genre": "research_article", 
    "id": "sg:pub.10.1007/s00015-004-1124-7", 
    "inLanguage": [
      "en"
    ], 
    "isAccessibleForFree": false, 
    "isPartOf": [
      {
        "id": "sg:journal.1135924", 
        "issn": [
          "0012-9402", 
          "1420-9128"
        ], 
        "name": "Eclogae Geologicae Helvetiae", 
        "type": "Periodical"
      }, 
      {
        "issueNumber": "2", 
        "type": "PublicationIssue"
      }, 
      {
        "type": "PublicationVolume", 
        "volumeNumber": "97"
      }
    ], 
    "name": "D\u00e9pliage 3-D des anticlinaux bordant le synclinal ferm\u00e9 de la vall\u00e9e des Ponts, Jura central, Suisse", 
    "pagination": "279-291", 
    "productId": [
      {
        "name": "readcube_id", 
        "type": "PropertyValue", 
        "value": [
          "aab92f2dc98d1aec26d3b9bb9a6badf983e6de74495f84cfe81eb095d7137550"
        ]
      }, 
      {
        "name": "doi", 
        "type": "PropertyValue", 
        "value": [
          "10.1007/s00015-004-1124-7"
        ]
      }, 
      {
        "name": "dimensions_id", 
        "type": "PropertyValue", 
        "value": [
          "pub.1035838701"
        ]
      }
    ], 
    "sameAs": [
      "https://doi.org/10.1007/s00015-004-1124-7", 
      "https://app.dimensions.ai/details/publication/pub.1035838701"
    ], 
    "sdDataset": "articles", 
    "sdDatePublished": "2019-04-10T21:33", 
    "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/v90/0000000001_0000000264/records_8687_00000496.jsonl", 
    "type": "ScholarlyArticle", 
    "url": "http://link.springer.com/10.1007/s00015-004-1124-7"
  }
]
 

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/s00015-004-1124-7'

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/s00015-004-1124-7'

Turtle is a human-readable linked data format.

curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1007/s00015-004-1124-7'

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

curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1007/s00015-004-1124-7'


 

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

102 TRIPLES      21 PREDICATES      35 URIs      19 LITERALS      7 BLANK NODES

Subject Predicate Object
1 sg:pub.10.1007/s00015-004-1124-7 schema:about anzsrc-for:04
2 anzsrc-for:0403
3 schema:author N5f297660446843ea915102c9b6f2b9c2
4 schema:citation sg:pub.10.1007/bf02986582
5 https://doi.org/10.1016/0040-1951(91)90363-w
6 https://doi.org/10.1016/s0012-821x(99)00238-1
7 https://doi.org/10.1016/s0191-8141(96)00104-6
8 https://doi.org/10.1016/s0191-8141(99)00021-8
9 https://doi.org/10.1029/2002jb002270
10 https://doi.org/10.1144/gsl.sp.1998.134.01.13
11 https://doi.org/10.1146/annurev.ea.18.050190.000415
12 schema:datePublished 2004-08
13 schema:datePublishedReg 2004-08-01
14 schema:description The Ponts valley syncline is a closed basin within the Neuchâtel Jura fold and thrust belt. This syncline, apparently uplifted to an altitude of around 1000m is closed in the SW by an anticline with an oblique WNW-ESE direction. The 3-D geometry of the entire structure is examined and unfolded in detail. This syncline is filled with an unexpectedly thick series (~400m) of Tertiairy Molasse, as revealed by the CS-AMT (controlled source audio-magneto-telluric) and a reflexion seismic line. The latter also documents internal compressional structures within the well layered upper freshwater Molasse series. The 3-D configuration of the top Malm limestones has been constructed for the entire area based on new detailed geologic and structural mapping, hundreds of dip measurements, as well as geophysical data. The Malm marker bed displays three distinct types of structures: 1) Thrust faults with shallow dips, vergent to the NW and/or SE that are associated with folds interpreted as fault bend folds; 2) high angle inverse faults, mostly with a SE vergence are interpreted as inverted normal faults, inherited from a modest Oligo-Miocene extensional phase in a NW-SE direction; and 3) tear faults with a dominant N-S direction, probably inherited from an Oligocene extensional phase in association with the opening of the Rhine and Bresse grabens. Tear faults accommodate important lateral changes in fold geometry during the Late Miocene main folding-and-thrusting phase. All deformations are easily explained in an entirely thin-skinned fashion, taking place above a thick detachment horizon within Triassic evaporite series.
15 schema:genre research_article
16 schema:inLanguage en
17 schema:isAccessibleForFree false
18 schema:isPartOf N4c844561b6a547108242919ab4ae8ea4
19 Nfc8922514e70494e93f8a902608190d5
20 sg:journal.1135924
21 schema:name Dépliage 3-D des anticlinaux bordant le synclinal fermé de la vallée des Ponts, Jura central, Suisse
22 schema:pagination 279-291
23 schema:productId N6882077e982d45e4a1a4c2fa8a06f6f1
24 N9bd4f9cbf97a448c8c428fb46d827db3
25 Nf998fa6fcf4745148d590710cd7bd829
26 schema:sameAs https://app.dimensions.ai/details/publication/pub.1035838701
27 https://doi.org/10.1007/s00015-004-1124-7
28 schema:sdDatePublished 2019-04-10T21:33
29 schema:sdLicense https://scigraph.springernature.com/explorer/license/
30 schema:sdPublisher Nfcec6d5dc85f488da2c623d339d89c3f
31 schema:url http://link.springer.com/10.1007/s00015-004-1124-7
32 sgo:license sg:explorer/license/
33 sgo:sdDataset articles
34 rdf:type schema:ScholarlyArticle
35 N287fe899b222488c805b69bc9c67ed70 rdf:first sg:person.07717024445.64
36 rdf:rest N3d4dd0be898244ab9070558ee7374616
37 N3d4dd0be898244ab9070558ee7374616 rdf:first sg:person.0666663007.59
38 rdf:rest rdf:nil
39 N421ce23939c649a7af3ae3dd1c3a3a5e schema:affiliation N6220c1b0a36a4f30a64344b669a21cd7
40 schema:familyName Valley
41 schema:givenName Benoît
42 rdf:type schema:Person
43 N4c844561b6a547108242919ab4ae8ea4 schema:issueNumber 2
44 rdf:type schema:PublicationIssue
45 N5f297660446843ea915102c9b6f2b9c2 rdf:first N421ce23939c649a7af3ae3dd1c3a3a5e
46 rdf:rest N287fe899b222488c805b69bc9c67ed70
47 N6220c1b0a36a4f30a64344b669a21cd7 schema:name Institut de Géologie, Rue E.Argand 11, Case Postale, 2007, Neuchâtel, Switzerland
48 rdf:type schema:Organization
49 N6882077e982d45e4a1a4c2fa8a06f6f1 schema:name readcube_id
50 schema:value aab92f2dc98d1aec26d3b9bb9a6badf983e6de74495f84cfe81eb095d7137550
51 rdf:type schema:PropertyValue
52 N9bd4f9cbf97a448c8c428fb46d827db3 schema:name doi
53 schema:value 10.1007/s00015-004-1124-7
54 rdf:type schema:PropertyValue
55 Nad7df11d7969451d8c7cfd8dee20d654 schema:name Institut de Géologie, Rue E.Argand 11, Case Postale, 2007, Neuchâtel, Switzerland
56 rdf:type schema:Organization
57 Ne79f26178e8e4c0aa1483c0a1480b52e schema:name Institut de Géologie, Rue E.Argand 11, Case Postale, 2007, Neuchâtel, Switzerland
58 rdf:type schema:Organization
59 Nf998fa6fcf4745148d590710cd7bd829 schema:name dimensions_id
60 schema:value pub.1035838701
61 rdf:type schema:PropertyValue
62 Nfc8922514e70494e93f8a902608190d5 schema:volumeNumber 97
63 rdf:type schema:PublicationVolume
64 Nfcec6d5dc85f488da2c623d339d89c3f schema:name Springer Nature - SN SciGraph project
65 rdf:type schema:Organization
66 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
67 schema:name Earth Sciences
68 rdf:type schema:DefinedTerm
69 anzsrc-for:0403 schema:inDefinedTermSet anzsrc-for:
70 schema:name Geology
71 rdf:type schema:DefinedTerm
72 sg:journal.1135924 schema:issn 0012-9402
73 1420-9128
74 schema:name Eclogae Geologicae Helvetiae
75 rdf:type schema:Periodical
76 sg:person.0666663007.59 schema:affiliation Nad7df11d7969451d8c7cfd8dee20d654
77 schema:familyName Schnegg
78 schema:givenName Pierre-André
79 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.0666663007.59
80 rdf:type schema:Person
81 sg:person.07717024445.64 schema:affiliation Ne79f26178e8e4c0aa1483c0a1480b52e
82 schema:familyName Burkhard
83 schema:givenName Martin
84 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.07717024445.64
85 rdf:type schema:Person
86 sg:pub.10.1007/bf02986582 schema:sameAs https://app.dimensions.ai/details/publication/pub.1044193617
87 https://doi.org/10.1007/bf02986582
88 rdf:type schema:CreativeWork
89 https://doi.org/10.1016/0040-1951(91)90363-w schema:sameAs https://app.dimensions.ai/details/publication/pub.1018837617
90 rdf:type schema:CreativeWork
91 https://doi.org/10.1016/s0012-821x(99)00238-1 schema:sameAs https://app.dimensions.ai/details/publication/pub.1030287983
92 rdf:type schema:CreativeWork
93 https://doi.org/10.1016/s0191-8141(96)00104-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1021579079
94 rdf:type schema:CreativeWork
95 https://doi.org/10.1016/s0191-8141(99)00021-8 schema:sameAs https://app.dimensions.ai/details/publication/pub.1040845579
96 rdf:type schema:CreativeWork
97 https://doi.org/10.1029/2002jb002270 schema:sameAs https://app.dimensions.ai/details/publication/pub.1023483548
98 rdf:type schema:CreativeWork
99 https://doi.org/10.1144/gsl.sp.1998.134.01.13 schema:sameAs https://app.dimensions.ai/details/publication/pub.1033272475
100 rdf:type schema:CreativeWork
101 https://doi.org/10.1146/annurev.ea.18.050190.000415 schema:sameAs https://app.dimensions.ai/details/publication/pub.1001712011
102 rdf:type schema:CreativeWork
 




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


...