The structure and formation conditions of the upper Jurassic succession in the area of Mount Pakhkal-Kaya (Crimea)
It has been found that the section in Mount Pakhkal-Kaya consists of three structural units separated by almost bedding-plane faults presumably arranged in a normal stratigraphic succession: conglomerate succession (I, ?J 3 ox (Oxfordian)), carbonate succession (II, ?J 3 km(Kimmeridgian)-tt(Tithonia...
Gespeichert in:
| Veröffentlicht in: | Moscow University geology bulletin 2010-02, Vol.65 (1), p.17-26 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 26 |
|---|---|
| container_issue | 1 |
| container_start_page | 17 |
| container_title | Moscow University geology bulletin |
| container_volume | 65 |
| creator | Baraboshkin, E. Yu Piskunov, V. K. |
| description | It has been found that the section in Mount Pakhkal-Kaya consists of three structural units separated by almost bedding-plane faults presumably arranged in a normal stratigraphic succession: conglomerate succession (I, ?J
3
ox (Oxfordian)), carbonate succession (II, ?J
3
km(Kimmeridgian)-tt(Tithonian)), and a conglomerate-breccia unit) (III, J3km-tt). Each of these successions corresponds to a certain stage of basin evolution, viz., formation of a Gilbert-type delta and the accumulation of a carbonate platform rimmed with a shoal and destruction of the platform margin during its periodic exposures. |
| doi_str_mv | 10.3103/S0145875210010023 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_598321304</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2005437981</sourcerecordid><originalsourceid>FETCH-LOGICAL-c245t-a2dadf50f5c11c903f8c289e5a53c770b076fbe748218c8488411320ecad5b6f3</originalsourceid><addsrcrecordid>eNp1kE1LxDAQhoMouK7-AG_Bkx6q-dymR1n8XlFwPZdpmrjdj6YmzWH_vakreBBhYF6Y531nGIROKbnklPCrN0KFVLlklJBUjO-hES24yJTgk300GsbZMD9ERyEsCZGyEGSE_HxhcOh91H30BkNbY-v8BvrGtVi7tm4GFbCzuE9k7Drj8WP0EEKjcYham6QS27TfAHgDA_zsYtvjV1gtVrDOnmAL-Hzqm42Bi2N0YGEdzMlPH6P325v59D6bvdw9TK9nmWZC9hmwGmoriZWaUl0QbpVmqjASJNd5TiqST2xlcqEYVVoJpQSlnBGjoZbVxPIxOtvldt59RhP6cumib9PKUhaKM8qJSBDdQdq7ELyxZZeuBL8tKSmHz5Z_Pps8bOcJiW0_jP8N_t_0BSd3eoM</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>598321304</pqid></control><display><type>article</type><title>The structure and formation conditions of the upper Jurassic succession in the area of Mount Pakhkal-Kaya (Crimea)</title><source>SpringerLink Journals</source><creator>Baraboshkin, E. Yu ; Piskunov, V. K.</creator><creatorcontrib>Baraboshkin, E. Yu ; Piskunov, V. K.</creatorcontrib><description>It has been found that the section in Mount Pakhkal-Kaya consists of three structural units separated by almost bedding-plane faults presumably arranged in a normal stratigraphic succession: conglomerate succession (I, ?J
3
ox (Oxfordian)), carbonate succession (II, ?J
3
km(Kimmeridgian)-tt(Tithonian)), and a conglomerate-breccia unit) (III, J3km-tt). Each of these successions corresponds to a certain stage of basin evolution, viz., formation of a Gilbert-type delta and the accumulation of a carbonate platform rimmed with a shoal and destruction of the platform margin during its periodic exposures.</description><identifier>ISSN: 0145-8752</identifier><identifier>EISSN: 1934-8436</identifier><identifier>DOI: 10.3103/S0145875210010023</identifier><language>eng</language><publisher>Heidelberg: Allerton Press, Inc</publisher><subject>Carbon ; Earth and Environmental Science ; Earth Sciences ; Geology ; Jurassic ; Mountains ; Petrology ; Stratigraphy</subject><ispartof>Moscow University geology bulletin, 2010-02, Vol.65 (1), p.17-26</ispartof><rights>Allerton Press, Inc. 2010</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c245t-a2dadf50f5c11c903f8c289e5a53c770b076fbe748218c8488411320ecad5b6f3</citedby><cites>FETCH-LOGICAL-c245t-a2dadf50f5c11c903f8c289e5a53c770b076fbe748218c8488411320ecad5b6f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.3103/S0145875210010023$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.3103/S0145875210010023$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Baraboshkin, E. Yu</creatorcontrib><creatorcontrib>Piskunov, V. K.</creatorcontrib><title>The structure and formation conditions of the upper Jurassic succession in the area of Mount Pakhkal-Kaya (Crimea)</title><title>Moscow University geology bulletin</title><addtitle>Moscow Univ. Geol. Bull</addtitle><description>It has been found that the section in Mount Pakhkal-Kaya consists of three structural units separated by almost bedding-plane faults presumably arranged in a normal stratigraphic succession: conglomerate succession (I, ?J
3
ox (Oxfordian)), carbonate succession (II, ?J
3
km(Kimmeridgian)-tt(Tithonian)), and a conglomerate-breccia unit) (III, J3km-tt). Each of these successions corresponds to a certain stage of basin evolution, viz., formation of a Gilbert-type delta and the accumulation of a carbonate platform rimmed with a shoal and destruction of the platform margin during its periodic exposures.</description><subject>Carbon</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Jurassic</subject><subject>Mountains</subject><subject>Petrology</subject><subject>Stratigraphy</subject><issn>0145-8752</issn><issn>1934-8436</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kE1LxDAQhoMouK7-AG_Bkx6q-dymR1n8XlFwPZdpmrjdj6YmzWH_vakreBBhYF6Y531nGIROKbnklPCrN0KFVLlklJBUjO-hES24yJTgk300GsbZMD9ERyEsCZGyEGSE_HxhcOh91H30BkNbY-v8BvrGtVi7tm4GFbCzuE9k7Drj8WP0EEKjcYham6QS27TfAHgDA_zsYtvjV1gtVrDOnmAL-Hzqm42Bi2N0YGEdzMlPH6P325v59D6bvdw9TK9nmWZC9hmwGmoriZWaUl0QbpVmqjASJNd5TiqST2xlcqEYVVoJpQSlnBGjoZbVxPIxOtvldt59RhP6cumib9PKUhaKM8qJSBDdQdq7ELyxZZeuBL8tKSmHz5Z_Pps8bOcJiW0_jP8N_t_0BSd3eoM</recordid><startdate>20100201</startdate><enddate>20100201</enddate><creator>Baraboshkin, E. Yu</creator><creator>Piskunov, V. K.</creator><general>Allerton Press, Inc</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20100201</creationdate><title>The structure and formation conditions of the upper Jurassic succession in the area of Mount Pakhkal-Kaya (Crimea)</title><author>Baraboshkin, E. Yu ; Piskunov, V. K.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c245t-a2dadf50f5c11c903f8c289e5a53c770b076fbe748218c8488411320ecad5b6f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Carbon</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Jurassic</topic><topic>Mountains</topic><topic>Petrology</topic><topic>Stratigraphy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Baraboshkin, E. Yu</creatorcontrib><creatorcontrib>Piskunov, V. K.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</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>Natural Science Collection (ProQuest)</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database (ProQuest)</collection><collection>Earth, Atmospheric & Aquatic Science Database</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 Basic</collection><jtitle>Moscow University geology bulletin</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Baraboshkin, E. Yu</au><au>Piskunov, V. K.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The structure and formation conditions of the upper Jurassic succession in the area of Mount Pakhkal-Kaya (Crimea)</atitle><jtitle>Moscow University geology bulletin</jtitle><stitle>Moscow Univ. Geol. Bull</stitle><date>2010-02-01</date><risdate>2010</risdate><volume>65</volume><issue>1</issue><spage>17</spage><epage>26</epage><pages>17-26</pages><issn>0145-8752</issn><eissn>1934-8436</eissn><abstract>It has been found that the section in Mount Pakhkal-Kaya consists of three structural units separated by almost bedding-plane faults presumably arranged in a normal stratigraphic succession: conglomerate succession (I, ?J
3
ox (Oxfordian)), carbonate succession (II, ?J
3
km(Kimmeridgian)-tt(Tithonian)), and a conglomerate-breccia unit) (III, J3km-tt). Each of these successions corresponds to a certain stage of basin evolution, viz., formation of a Gilbert-type delta and the accumulation of a carbonate platform rimmed with a shoal and destruction of the platform margin during its periodic exposures.</abstract><cop>Heidelberg</cop><pub>Allerton Press, Inc</pub><doi>10.3103/S0145875210010023</doi><tpages>10</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0145-8752 |
| ispartof | Moscow University geology bulletin, 2010-02, Vol.65 (1), p.17-26 |
| issn | 0145-8752 1934-8436 |
| language | eng |
| recordid | cdi_proquest_journals_598321304 |
| source | SpringerLink Journals |
| subjects | Carbon Earth and Environmental Science Earth Sciences Geology Jurassic Mountains Petrology Stratigraphy |
| title | The structure and formation conditions of the upper Jurassic succession in the area of Mount Pakhkal-Kaya (Crimea) |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-24T03%3A46%3A51IST&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=The%20structure%20and%20formation%20conditions%20of%20the%20upper%20Jurassic%20succession%20in%20the%20area%20of%20Mount%20Pakhkal-Kaya%20(Crimea)&rft.jtitle=Moscow%20University%20geology%20bulletin&rft.au=Baraboshkin,%20E.%20Yu&rft.date=2010-02-01&rft.volume=65&rft.issue=1&rft.spage=17&rft.epage=26&rft.pages=17-26&rft.issn=0145-8752&rft.eissn=1934-8436&rft_id=info:doi/10.3103/S0145875210010023&rft_dat=%3Cproquest_cross%3E2005437981%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=598321304&rft_id=info:pmid/&rfr_iscdi=true |