A 3D, map based approach to reconstruct and calibrate palaeo-bathymetries – Testing the Cretaceous water depth of the Hammerfest Basin, southwestern Barents Sea
A new 3D approach to quantify and calibrate palaeo-water depth (PWD) has been applied to evaluate the Aptian to Maastrichtian/Danian (Cretaceous) bathymetric development in a sub-basin scale within the Hammerfest Basin, southwestern Barents Sea. The results indicate PWD's varying between ca. 20...
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Veröffentlicht in: | Continental shelf research 2015-04, Vol.97, p.21-31 |
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creator | Emmel, B. de Jager, G. Zieba, K. Kurtev, K. Grøver, A. Lothe, A. Lippard, S.J. Roli, O.A. |
description | A new 3D approach to quantify and calibrate palaeo-water depth (PWD) has been applied to evaluate the Aptian to Maastrichtian/Danian (Cretaceous) bathymetric development in a sub-basin scale within the Hammerfest Basin, southwestern Barents Sea. The results indicate PWD's varying between ca. 200m and 95m, recording a local sea-level decrease of ca. 105m. A calibration against shale volume based on gamma-ray logs from four exploration wells indicates a model sensitivity of ca. +50m and −150m. These results are in agreement with empirical PWD estimates obtained from sedimentological and micropalaeontological observations. A comparison with the global eustatic sea level curve indicates that the PWD decrease in the Hammerfest Basin contradicts the general, global trend indicating a primary control by local tectonics such as differential subsidence and uplift along the evolving continental margin offshore north-west Norway.
•A new approach to reconstruct and calibrate palaeo-bathymetries was tested in the Barents Sea.•Modeled Cretaceous bathymetry of the Hammerfest Basin is in agreement with estimates based on sedimentology and micropalaeontology.•Late Cretaceous bathymetric modification as a response to uplift in the Hammerfest Basin. |
doi_str_mv | 10.1016/j.csr.2015.02.003 |
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•A new approach to reconstruct and calibrate palaeo-bathymetries was tested in the Barents Sea.•Modeled Cretaceous bathymetry of the Hammerfest Basin is in agreement with estimates based on sedimentology and micropalaeontology.•Late Cretaceous bathymetric modification as a response to uplift in the Hammerfest Basin.</description><identifier>ISSN: 0278-4343</identifier><identifier>EISSN: 1873-6955</identifier><identifier>DOI: 10.1016/j.csr.2015.02.003</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Barents Sea ; Basin modeling ; Basins ; Calibration ; Continental shelves ; Cretaceous ; Estimates ; Hammerfest Basin ; Marine ; Palaeo-bathymetry ; Recording ; Sea level ; Three dimensional</subject><ispartof>Continental shelf research, 2015-04, Vol.97, p.21-31</ispartof><rights>2015 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a386t-fa23910e57e2fe99068a5605502846b96dda9432af8b3debac59ed01d758aefa3</citedby><cites>FETCH-LOGICAL-a386t-fa23910e57e2fe99068a5605502846b96dda9432af8b3debac59ed01d758aefa3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0278434315000424$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids></links><search><creatorcontrib>Emmel, B.</creatorcontrib><creatorcontrib>de Jager, G.</creatorcontrib><creatorcontrib>Zieba, K.</creatorcontrib><creatorcontrib>Kurtev, K.</creatorcontrib><creatorcontrib>Grøver, A.</creatorcontrib><creatorcontrib>Lothe, A.</creatorcontrib><creatorcontrib>Lippard, S.J.</creatorcontrib><creatorcontrib>Roli, O.A.</creatorcontrib><title>A 3D, map based approach to reconstruct and calibrate palaeo-bathymetries – Testing the Cretaceous water depth of the Hammerfest Basin, southwestern Barents Sea</title><title>Continental shelf research</title><description>A new 3D approach to quantify and calibrate palaeo-water depth (PWD) has been applied to evaluate the Aptian to Maastrichtian/Danian (Cretaceous) bathymetric development in a sub-basin scale within the Hammerfest Basin, southwestern Barents Sea. The results indicate PWD's varying between ca. 200m and 95m, recording a local sea-level decrease of ca. 105m. A calibration against shale volume based on gamma-ray logs from four exploration wells indicates a model sensitivity of ca. +50m and −150m. These results are in agreement with empirical PWD estimates obtained from sedimentological and micropalaeontological observations. A comparison with the global eustatic sea level curve indicates that the PWD decrease in the Hammerfest Basin contradicts the general, global trend indicating a primary control by local tectonics such as differential subsidence and uplift along the evolving continental margin offshore north-west Norway.
•A new approach to reconstruct and calibrate palaeo-bathymetries was tested in the Barents Sea.•Modeled Cretaceous bathymetry of the Hammerfest Basin is in agreement with estimates based on sedimentology and micropalaeontology.•Late Cretaceous bathymetric modification as a response to uplift in the Hammerfest Basin.</description><subject>Barents Sea</subject><subject>Basin modeling</subject><subject>Basins</subject><subject>Calibration</subject><subject>Continental shelves</subject><subject>Cretaceous</subject><subject>Estimates</subject><subject>Hammerfest Basin</subject><subject>Marine</subject><subject>Palaeo-bathymetry</subject><subject>Recording</subject><subject>Sea level</subject><subject>Three dimensional</subject><issn>0278-4343</issn><issn>1873-6955</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNqNkUtuFEEMhluISAwJB2DnJYt04-qa6odYheERpEhZENYld5WbrlG_qKohyo47cAOOlpNQw7BGeGPJ_n_L9pdlLwUWAkX1el-Y4IsShSqwLBDlk2wjmlrmVavU02yDZd3kW7mVz7LnIewRsa7aepP9ugL57hImWqGjwBZoXf1CZoC4gGezzCH6g4lAswVDo-s8RYaVRuIl7ygODxNH7zjA44-fcMchuvkrxIFh5zmS4eUQ4D55PFhe4wBL_6d7TdPEvk96eEvBzZcQlkMc7lOB_ZxqnucY4DPTRXbW0xj4xd98nn358P5ud53f3H78tLu6yUk2Vcx7KmUrkFXNZc9ti1VDqkKlsGy2VddW1lK7lSX1TSctd2RUyxaFrVVD3JM8z16d5qYHfDukPfTkguFxpPl4hBZ1jVJI1aj_kMqykSkwScVJavwSguder95N5B-0QH1Ep_c6odNHdBpLndAlz5uTh9O53x17HYzj2bB1CUnUdnH_cP8GF4SkiA</recordid><startdate>20150401</startdate><enddate>20150401</enddate><creator>Emmel, B.</creator><creator>de Jager, G.</creator><creator>Zieba, K.</creator><creator>Kurtev, K.</creator><creator>Grøver, A.</creator><creator>Lothe, A.</creator><creator>Lippard, S.J.</creator><creator>Roli, O.A.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20150401</creationdate><title>A 3D, map based approach to reconstruct and calibrate palaeo-bathymetries – Testing the Cretaceous water depth of the Hammerfest Basin, southwestern Barents Sea</title><author>Emmel, B. ; de Jager, G. ; Zieba, K. ; Kurtev, K. ; Grøver, A. ; Lothe, A. ; Lippard, S.J. ; Roli, O.A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a386t-fa23910e57e2fe99068a5605502846b96dda9432af8b3debac59ed01d758aefa3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Barents Sea</topic><topic>Basin modeling</topic><topic>Basins</topic><topic>Calibration</topic><topic>Continental shelves</topic><topic>Cretaceous</topic><topic>Estimates</topic><topic>Hammerfest Basin</topic><topic>Marine</topic><topic>Palaeo-bathymetry</topic><topic>Recording</topic><topic>Sea level</topic><topic>Three dimensional</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Emmel, B.</creatorcontrib><creatorcontrib>de Jager, G.</creatorcontrib><creatorcontrib>Zieba, K.</creatorcontrib><creatorcontrib>Kurtev, K.</creatorcontrib><creatorcontrib>Grøver, A.</creatorcontrib><creatorcontrib>Lothe, A.</creatorcontrib><creatorcontrib>Lippard, S.J.</creatorcontrib><creatorcontrib>Roli, O.A.</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Continental shelf research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Emmel, B.</au><au>de Jager, G.</au><au>Zieba, K.</au><au>Kurtev, K.</au><au>Grøver, A.</au><au>Lothe, A.</au><au>Lippard, S.J.</au><au>Roli, O.A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A 3D, map based approach to reconstruct and calibrate palaeo-bathymetries – Testing the Cretaceous water depth of the Hammerfest Basin, southwestern Barents Sea</atitle><jtitle>Continental shelf research</jtitle><date>2015-04-01</date><risdate>2015</risdate><volume>97</volume><spage>21</spage><epage>31</epage><pages>21-31</pages><issn>0278-4343</issn><eissn>1873-6955</eissn><abstract>A new 3D approach to quantify and calibrate palaeo-water depth (PWD) has been applied to evaluate the Aptian to Maastrichtian/Danian (Cretaceous) bathymetric development in a sub-basin scale within the Hammerfest Basin, southwestern Barents Sea. The results indicate PWD's varying between ca. 200m and 95m, recording a local sea-level decrease of ca. 105m. A calibration against shale volume based on gamma-ray logs from four exploration wells indicates a model sensitivity of ca. +50m and −150m. These results are in agreement with empirical PWD estimates obtained from sedimentological and micropalaeontological observations. A comparison with the global eustatic sea level curve indicates that the PWD decrease in the Hammerfest Basin contradicts the general, global trend indicating a primary control by local tectonics such as differential subsidence and uplift along the evolving continental margin offshore north-west Norway.
•A new approach to reconstruct and calibrate palaeo-bathymetries was tested in the Barents Sea.•Modeled Cretaceous bathymetry of the Hammerfest Basin is in agreement with estimates based on sedimentology and micropalaeontology.•Late Cretaceous bathymetric modification as a response to uplift in the Hammerfest Basin.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.csr.2015.02.003</doi><tpages>11</tpages></addata></record> |
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subjects | Barents Sea Basin modeling Basins Calibration Continental shelves Cretaceous Estimates Hammerfest Basin Marine Palaeo-bathymetry Recording Sea level Three dimensional |
title | A 3D, map based approach to reconstruct and calibrate palaeo-bathymetries – Testing the Cretaceous water depth of the Hammerfest Basin, southwestern Barents Sea |
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