Towards deciphering the Cenozoic evolution of the East Pisco Basin (southern Peru)
The Cenozoic succession of the East Pisco Basin preserves the sedimentary record of several episodes of deformation of the forearc crust along the Peruvian margin. The 1:50,000 scale geological map presented here encompasses an area of about 1,000 km 2 lying astride the Ica River, and contributes to...
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| Veröffentlicht in: | Journal of maps 2022-12, Vol.18 (2), p.397-412 |
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| creator | Di Celma, C. Pierantoni, P.P. Volatili, T. Molli, G. Mazzoli, S. Sarti, G. Ciattoni, S. Bosio, G. Malinverno, E. Collareta, A. Gariboldi, K. Gioncada, A. Jablonska, D. Landini, W. Urbina, M. Bianucci, G. |
| description | The Cenozoic succession of the East Pisco Basin preserves the sedimentary record of several episodes of deformation of the forearc crust along the Peruvian margin. The 1:50,000 scale geological map presented here encompasses an area of about 1,000 km
2
lying astride the Ica River, and contributes to our understanding of the timing and mode of basin filling and deformation. Our novel two-fold megasequence framework provides a sound basis for establishing a first-order tectono-stratigraphic setting of the mid-Eocene-upper Miocene succession exposed in the study area. We interpret that the mid-Eocene to lower Oligocene succession studied in this work (megasequence P) was deposited in a single forearc basin, which was dissected into the present-day West and East Pisco basins by a fault-bounded basement high during the late Oligocene, and subsequently overlain by the Miocene fill of the East Pisco basin (megasequence N). |
| doi_str_mv | 10.1080/17445647.2022.2072780 |
| format | Article |
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lying astride the Ica River, and contributes to our understanding of the timing and mode of basin filling and deformation. Our novel two-fold megasequence framework provides a sound basis for establishing a first-order tectono-stratigraphic setting of the mid-Eocene-upper Miocene succession exposed in the study area. We interpret that the mid-Eocene to lower Oligocene succession studied in this work (megasequence P) was deposited in a single forearc basin, which was dissected into the present-day West and East Pisco basins by a fault-bounded basement high during the late Oligocene, and subsequently overlain by the Miocene fill of the East Pisco basin (megasequence N).</description><identifier>ISSN: 1744-5647</identifier><identifier>EISSN: 1744-5647</identifier><identifier>DOI: 10.1080/17445647.2022.2072780</identifier><language>eng</language><publisher>Abingdon: Taylor & Francis</publisher><subject>basin inversion ; Basins ; Cenozoic ; Deformation ; East Pisco Basin ; Eocene ; forearc basin ; Geologic mapping ; Geological mapping ; Geology ; Mapping ; Miocene ; Oligocene ; Sediments ; Stratigraphy</subject><ispartof>Journal of maps, 2022-12, Vol.18 (2), p.397-412</ispartof><rights>2022 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps 2022</rights><rights>2022 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-c451t-615e71f3e14e6432da145c1efcf431d79bdcdea1b64056a98b1cd48af5a0153f3</citedby><cites>FETCH-LOGICAL-c451t-615e71f3e14e6432da145c1efcf431d79bdcdea1b64056a98b1cd48af5a0153f3</cites><orcidid>0000-0001-7196-9888 ; 0000-0002-9124-5155 ; 0000-0001-5342-5086 ; 0000-0001-8067-4926 ; 0000-0002-6513-8882 ; 0000-0003-3911-9183 ; 0000-0001-9177-5706 ; 0000-0001-9488-8132 ; 0000-0001-7781-7981 ; 0000-0002-6327-4768 ; 0000-0002-5055-3282 ; 0000-0002-1898-9051 ; 0000-0002-8513-7377 ; 0000-0001-7105-0863 ; 0000-0002-1237-4689 ; 0000-0002-7978-7496</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.1080/17445647.2022.2072780$$EPDF$$P50$$Ginformaworld$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.1080/17445647.2022.2072780$$EHTML$$P50$$Ginformaworld$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,860,2096,27479,27901,27902,59116,59117</link.rule.ids></links><search><creatorcontrib>Di Celma, C.</creatorcontrib><creatorcontrib>Pierantoni, P.P.</creatorcontrib><creatorcontrib>Volatili, T.</creatorcontrib><creatorcontrib>Molli, G.</creatorcontrib><creatorcontrib>Mazzoli, S.</creatorcontrib><creatorcontrib>Sarti, G.</creatorcontrib><creatorcontrib>Ciattoni, S.</creatorcontrib><creatorcontrib>Bosio, G.</creatorcontrib><creatorcontrib>Malinverno, E.</creatorcontrib><creatorcontrib>Collareta, A.</creatorcontrib><creatorcontrib>Gariboldi, K.</creatorcontrib><creatorcontrib>Gioncada, A.</creatorcontrib><creatorcontrib>Jablonska, D.</creatorcontrib><creatorcontrib>Landini, W.</creatorcontrib><creatorcontrib>Urbina, M.</creatorcontrib><creatorcontrib>Bianucci, G.</creatorcontrib><title>Towards deciphering the Cenozoic evolution of the East Pisco Basin (southern Peru)</title><title>Journal of maps</title><description>The Cenozoic succession of the East Pisco Basin preserves the sedimentary record of several episodes of deformation of the forearc crust along the Peruvian margin. The 1:50,000 scale geological map presented here encompasses an area of about 1,000 km
2
lying astride the Ica River, and contributes to our understanding of the timing and mode of basin filling and deformation. Our novel two-fold megasequence framework provides a sound basis for establishing a first-order tectono-stratigraphic setting of the mid-Eocene-upper Miocene succession exposed in the study area. We interpret that the mid-Eocene to lower Oligocene succession studied in this work (megasequence P) was deposited in a single forearc basin, which was dissected into the present-day West and East Pisco basins by a fault-bounded basement high during the late Oligocene, and subsequently overlain by the Miocene fill of the East Pisco basin (megasequence N).</description><subject>basin inversion</subject><subject>Basins</subject><subject>Cenozoic</subject><subject>Deformation</subject><subject>East Pisco Basin</subject><subject>Eocene</subject><subject>forearc basin</subject><subject>Geologic mapping</subject><subject>Geological mapping</subject><subject>Geology</subject><subject>Mapping</subject><subject>Miocene</subject><subject>Oligocene</subject><subject>Sediments</subject><subject>Stratigraphy</subject><issn>1744-5647</issn><issn>1744-5647</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>0YH</sourceid><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><sourceid>DOA</sourceid><recordid>eNp9UU1LHEEQHYKBqPEnCA1e4mFNV39M996Mi0kEIRLMuanpD-1lnNp0zyjm12fWNSGnXKqK9169KnhNcwz8DLjlH8EopVtlzgQXYi5GGMvfNPtbfLEl9v6Z3zUHta4515Zbvd98v6UnLKGyEH3e3MeShzs23ke2igP9ouxZfKR-GjMNjNILc4l1ZDe5emIXWPPAPlSaZqIM7CaW6fR98zZhX-PRaz9sfny-vF19XVx_-3K1-nS98ErDuGhBRwNJRlCxVVIEBKU9xOSTkhDMsgs-RISuVVy3uLQd-KAsJo0ctEzysLna-QbCtduU_IDl2RFm9wJQuXNYxuz76JY-Cg3KWMOlEuBtJ7yUKiVv0HcAs9fJzmtT6OcU6-jWNJVhft8Jo63S2ig5q_RO5QvVWmL6exW420bh_kThtlG41yjmvfPdXh4SlQd8otIHN-JzTyUVHHyuTv7f4jc5o48D</recordid><startdate>20221201</startdate><enddate>20221201</enddate><creator>Di Celma, C.</creator><creator>Pierantoni, P.P.</creator><creator>Volatili, T.</creator><creator>Molli, G.</creator><creator>Mazzoli, S.</creator><creator>Sarti, G.</creator><creator>Ciattoni, S.</creator><creator>Bosio, G.</creator><creator>Malinverno, E.</creator><creator>Collareta, A.</creator><creator>Gariboldi, K.</creator><creator>Gioncada, A.</creator><creator>Jablonska, D.</creator><creator>Landini, W.</creator><creator>Urbina, M.</creator><creator>Bianucci, G.</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/0000-0001-7196-9888</orcidid><orcidid>https://orcid.org/0000-0002-9124-5155</orcidid><orcidid>https://orcid.org/0000-0001-5342-5086</orcidid><orcidid>https://orcid.org/0000-0001-8067-4926</orcidid><orcidid>https://orcid.org/0000-0002-6513-8882</orcidid><orcidid>https://orcid.org/0000-0003-3911-9183</orcidid><orcidid>https://orcid.org/0000-0001-9177-5706</orcidid><orcidid>https://orcid.org/0000-0001-9488-8132</orcidid><orcidid>https://orcid.org/0000-0001-7781-7981</orcidid><orcidid>https://orcid.org/0000-0002-6327-4768</orcidid><orcidid>https://orcid.org/0000-0002-5055-3282</orcidid><orcidid>https://orcid.org/0000-0002-1898-9051</orcidid><orcidid>https://orcid.org/0000-0002-8513-7377</orcidid><orcidid>https://orcid.org/0000-0001-7105-0863</orcidid><orcidid>https://orcid.org/0000-0002-1237-4689</orcidid><orcidid>https://orcid.org/0000-0002-7978-7496</orcidid></search><sort><creationdate>20221201</creationdate><title>Towards deciphering the Cenozoic evolution of the East Pisco Basin (southern Peru)</title><author>Di Celma, C. ; 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| subjects | basin inversion Basins Cenozoic Deformation East Pisco Basin Eocene forearc basin Geologic mapping Geological mapping Geology Mapping Miocene Oligocene Sediments Stratigraphy |
| title | Towards deciphering the Cenozoic evolution of the East Pisco Basin (southern Peru) |
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