Geology of the High Sillaro Valley (Northern Apennines of Italy)
We map the High Sillaro Valley, in the Northern Apennines of Italy. Here the Ligurian wedge overthrust the foredeep deposits of the Marnoso Arenacea formation - MA. The overthrusting occurred through a shear zone with components derived from the frontal part of the Ligurian wedge and interpreted as...
Gespeichert in:
| Veröffentlicht in: | Journal of maps 2020-12, Vol.16 (2), p.805-817 |
|---|---|
| Hauptverfasser: | , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 817 |
|---|---|
| container_issue | 2 |
| container_start_page | 805 |
| container_title | Journal of maps |
| container_volume | 16 |
| creator | Panini, Filippo Bettelli, Giuseppe Carlini, Mirko Fioroni, Chiara Nirta, Giuseppe Remitti, Francesca |
| description | We map the High Sillaro Valley, in the Northern Apennines of Italy. Here the Ligurian wedge overthrust the foredeep deposits of the Marnoso Arenacea formation - MA. The overthrusting occurred through a shear zone with components derived from the frontal part of the Ligurian wedge and interpreted as a tectonic mélange (Sestola-Vidiciatico Tectonic unit - SVU) here subdivided into two different subunits structurally independent one from the other. In the area, the Visignano chaotic body (VIS) constitutes an intercalation within the Serravallian-Tortonian MA and derives, as the SVU, from the frontal part of the Ligurian wedge. We performed a detailed investigation of the components of the VIS that helps to better define the architecture of the frontal part of the Ligurian wedge and to constrain the timing of the deformation phases affecting this portion of the Northern Apennines during the middle-late Miocene. |
| doi_str_mv | 10.1080/17445647.2020.1832926 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1080_17445647_2020_1832926</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><doaj_id>oai_doaj_org_article_cb00bb52df634f1ca70a3e54575e61ea</doaj_id><sourcerecordid>2476107330</sourcerecordid><originalsourceid>FETCH-LOGICAL-a474t-c09383becd7232165e2f836074fece1ca5f7f6f5c88a5f8fd3fdeb78f8882d6b3</originalsourceid><addsrcrecordid>eNp9kE1Lw0AQhoMoWKs_QQh40UPqZr97aynaFooe_Lgum81sm7LN1k2K5N-bmCqePM3wzjvPDG8UXadolCKJ7lNBKeNUjDDCrSQJHmN-Eg06PekGp3_68-iiqrYIMYkkG0STOXjn103sbVxvIF4U6038Ujing4_ftXPQxLdPPrSzUMbTPZRlUULV2Ze1ds3dZXRmtavg6liH0dvjw-tskaye58vZdJVoKmidGDQmkmRgcoEJTjkDbCXhSFALBlKjmRWWW2akbFtpc2JzyIS0Ukqc84wMo2XPzb3eqn0odjo0yutCfQs-rJUOdWEcKJMhlGUM55YTalu2QJoAo0ww4CnolnXTs_bBfxygqtXWH0LZvq8wFTxFghDUuljvMsFXVQD7ezVFqgte_QSvuuDVMfh2b9LvFaX1Yac_fXC5qnXjfLBBl6aoFPkf8QVjf4it</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2476107330</pqid></control><display><type>article</type><title>Geology of the High Sillaro Valley (Northern Apennines of Italy)</title><source>Taylor & Francis Open Access</source><source>DOAJ Directory of Open Access Journals</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><creator>Panini, Filippo ; Bettelli, Giuseppe ; Carlini, Mirko ; Fioroni, Chiara ; Nirta, Giuseppe ; Remitti, Francesca</creator><creatorcontrib>Panini, Filippo ; Bettelli, Giuseppe ; Carlini, Mirko ; Fioroni, Chiara ; Nirta, Giuseppe ; Remitti, Francesca</creatorcontrib><description>We map the High Sillaro Valley, in the Northern Apennines of Italy. Here the Ligurian wedge overthrust the foredeep deposits of the Marnoso Arenacea formation - MA. The overthrusting occurred through a shear zone with components derived from the frontal part of the Ligurian wedge and interpreted as a tectonic mélange (Sestola-Vidiciatico Tectonic unit - SVU) here subdivided into two different subunits structurally independent one from the other. In the area, the Visignano chaotic body (VIS) constitutes an intercalation within the Serravallian-Tortonian MA and derives, as the SVU, from the frontal part of the Ligurian wedge. We performed a detailed investigation of the components of the VIS that helps to better define the architecture of the frontal part of the Ligurian wedge and to constrain the timing of the deformation phases affecting this portion of the Northern Apennines during the middle-late Miocene.</description><identifier>ISSN: 1744-5647</identifier><identifier>EISSN: 1744-5647</identifier><identifier>DOI: 10.1080/17445647.2020.1832926</identifier><language>eng</language><publisher>Abingdon: Taylor & Francis</publisher><subject>Alliances ; Geology ; Miocene ; mélange ; Northern Apennines ; orogenic wedge ; Shear zone ; Sillaro Valley ; Tectonics ; Valleys</subject><ispartof>Journal of maps, 2020-12, Vol.16 (2), p.805-817</ispartof><rights>2020 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps 2020</rights><rights>2020 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps. This work is licensed under the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a474t-c09383becd7232165e2f836074fece1ca5f7f6f5c88a5f8fd3fdeb78f8882d6b3</citedby><cites>FETCH-LOGICAL-a474t-c09383becd7232165e2f836074fece1ca5f7f6f5c88a5f8fd3fdeb78f8882d6b3</cites><orcidid>0000-0002-0720-1927 ; 0000-0002-4319-9115 ; 0000-0003-1274-7067 ; 0000-0003-0514-5615 ; 0000-0002-7840-8992</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.1080/17445647.2020.1832926$$EPDF$$P50$$Ginformaworld$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.1080/17445647.2020.1832926$$EHTML$$P50$$Ginformaworld$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,864,2100,27500,27922,27923,59141,59142</link.rule.ids></links><search><creatorcontrib>Panini, Filippo</creatorcontrib><creatorcontrib>Bettelli, Giuseppe</creatorcontrib><creatorcontrib>Carlini, Mirko</creatorcontrib><creatorcontrib>Fioroni, Chiara</creatorcontrib><creatorcontrib>Nirta, Giuseppe</creatorcontrib><creatorcontrib>Remitti, Francesca</creatorcontrib><title>Geology of the High Sillaro Valley (Northern Apennines of Italy)</title><title>Journal of maps</title><description>We map the High Sillaro Valley, in the Northern Apennines of Italy. Here the Ligurian wedge overthrust the foredeep deposits of the Marnoso Arenacea formation - MA. The overthrusting occurred through a shear zone with components derived from the frontal part of the Ligurian wedge and interpreted as a tectonic mélange (Sestola-Vidiciatico Tectonic unit - SVU) here subdivided into two different subunits structurally independent one from the other. In the area, the Visignano chaotic body (VIS) constitutes an intercalation within the Serravallian-Tortonian MA and derives, as the SVU, from the frontal part of the Ligurian wedge. We performed a detailed investigation of the components of the VIS that helps to better define the architecture of the frontal part of the Ligurian wedge and to constrain the timing of the deformation phases affecting this portion of the Northern Apennines during the middle-late Miocene.</description><subject>Alliances</subject><subject>Geology</subject><subject>Miocene</subject><subject>mélange</subject><subject>Northern Apennines</subject><subject>orogenic wedge</subject><subject>Shear zone</subject><subject>Sillaro Valley</subject><subject>Tectonics</subject><subject>Valleys</subject><issn>1744-5647</issn><issn>1744-5647</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>0YH</sourceid><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><sourceid>DOA</sourceid><recordid>eNp9kE1Lw0AQhoMoWKs_QQh40UPqZr97aynaFooe_Lgum81sm7LN1k2K5N-bmCqePM3wzjvPDG8UXadolCKJ7lNBKeNUjDDCrSQJHmN-Eg06PekGp3_68-iiqrYIMYkkG0STOXjn103sbVxvIF4U6038Ujing4_ftXPQxLdPPrSzUMbTPZRlUULV2Ze1ds3dZXRmtavg6liH0dvjw-tskaye58vZdJVoKmidGDQmkmRgcoEJTjkDbCXhSFALBlKjmRWWW2akbFtpc2JzyIS0Ukqc84wMo2XPzb3eqn0odjo0yutCfQs-rJUOdWEcKJMhlGUM55YTalu2QJoAo0ww4CnolnXTs_bBfxygqtXWH0LZvq8wFTxFghDUuljvMsFXVQD7ezVFqgte_QSvuuDVMfh2b9LvFaX1Yac_fXC5qnXjfLBBl6aoFPkf8QVjf4it</recordid><startdate>20201209</startdate><enddate>20201209</enddate><creator>Panini, Filippo</creator><creator>Bettelli, Giuseppe</creator><creator>Carlini, Mirko</creator><creator>Fioroni, Chiara</creator><creator>Nirta, Giuseppe</creator><creator>Remitti, Francesca</creator><general>Taylor & Francis</general><general>Taylor & Francis Ltd</general><general>Taylor & Francis Group</general><scope>0YH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7XB</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>M2O</scope><scope>MBDVC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>Q9U</scope><scope>SOI</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0002-0720-1927</orcidid><orcidid>https://orcid.org/0000-0002-4319-9115</orcidid><orcidid>https://orcid.org/0000-0003-1274-7067</orcidid><orcidid>https://orcid.org/0000-0003-0514-5615</orcidid><orcidid>https://orcid.org/0000-0002-7840-8992</orcidid></search><sort><creationdate>20201209</creationdate><title>Geology of the High Sillaro Valley (Northern Apennines of Italy)</title><author>Panini, Filippo ; Bettelli, Giuseppe ; Carlini, Mirko ; Fioroni, Chiara ; Nirta, Giuseppe ; Remitti, Francesca</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a474t-c09383becd7232165e2f836074fece1ca5f7f6f5c88a5f8fd3fdeb78f8882d6b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Alliances</topic><topic>Geology</topic><topic>Miocene</topic><topic>mélange</topic><topic>Northern Apennines</topic><topic>orogenic wedge</topic><topic>Shear zone</topic><topic>Sillaro Valley</topic><topic>Tectonics</topic><topic>Valleys</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Panini, Filippo</creatorcontrib><creatorcontrib>Bettelli, Giuseppe</creatorcontrib><creatorcontrib>Carlini, Mirko</creatorcontrib><creatorcontrib>Fioroni, Chiara</creatorcontrib><creatorcontrib>Nirta, Giuseppe</creatorcontrib><creatorcontrib>Remitti, Francesca</creatorcontrib><collection>Taylor & Francis Open Access</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Research Library</collection><collection>Research Library (Corporate)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Journal of maps</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Panini, Filippo</au><au>Bettelli, Giuseppe</au><au>Carlini, Mirko</au><au>Fioroni, Chiara</au><au>Nirta, Giuseppe</au><au>Remitti, Francesca</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geology of the High Sillaro Valley (Northern Apennines of Italy)</atitle><jtitle>Journal of maps</jtitle><date>2020-12-09</date><risdate>2020</risdate><volume>16</volume><issue>2</issue><spage>805</spage><epage>817</epage><pages>805-817</pages><issn>1744-5647</issn><eissn>1744-5647</eissn><abstract>We map the High Sillaro Valley, in the Northern Apennines of Italy. Here the Ligurian wedge overthrust the foredeep deposits of the Marnoso Arenacea formation - MA. The overthrusting occurred through a shear zone with components derived from the frontal part of the Ligurian wedge and interpreted as a tectonic mélange (Sestola-Vidiciatico Tectonic unit - SVU) here subdivided into two different subunits structurally independent one from the other. In the area, the Visignano chaotic body (VIS) constitutes an intercalation within the Serravallian-Tortonian MA and derives, as the SVU, from the frontal part of the Ligurian wedge. We performed a detailed investigation of the components of the VIS that helps to better define the architecture of the frontal part of the Ligurian wedge and to constrain the timing of the deformation phases affecting this portion of the Northern Apennines during the middle-late Miocene.</abstract><cop>Abingdon</cop><pub>Taylor & Francis</pub><doi>10.1080/17445647.2020.1832926</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-0720-1927</orcidid><orcidid>https://orcid.org/0000-0002-4319-9115</orcidid><orcidid>https://orcid.org/0000-0003-1274-7067</orcidid><orcidid>https://orcid.org/0000-0003-0514-5615</orcidid><orcidid>https://orcid.org/0000-0002-7840-8992</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1744-5647 |
| ispartof | Journal of maps, 2020-12, Vol.16 (2), p.805-817 |
| issn | 1744-5647 1744-5647 |
| language | eng |
| recordid | cdi_crossref_primary_10_1080_17445647_2020_1832926 |
| source | Taylor & Francis Open Access; DOAJ Directory of Open Access Journals; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Alliances Geology Miocene mélange Northern Apennines orogenic wedge Shear zone Sillaro Valley Tectonics Valleys |
| title | Geology of the High Sillaro Valley (Northern Apennines of Italy) |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-09T19%3A47%3A47IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Geology%20of%20the%20High%20Sillaro%20Valley%20(Northern%20Apennines%20of%20Italy)&rft.jtitle=Journal%20of%20maps&rft.au=Panini,%20Filippo&rft.date=2020-12-09&rft.volume=16&rft.issue=2&rft.spage=805&rft.epage=817&rft.pages=805-817&rft.issn=1744-5647&rft.eissn=1744-5647&rft_id=info:doi/10.1080/17445647.2020.1832926&rft_dat=%3Cproquest_cross%3E2476107330%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2476107330&rft_id=info:pmid/&rft_doaj_id=oai_doaj_org_article_cb00bb52df634f1ca70a3e54575e61ea&rfr_iscdi=true |