Facies and sedimentology of a carbonate delta drift (Miocene, Maldives)
Abstract The identification of sediment drifts typically relies on interpretation of reflection seismic data sets. This study sedimentologically analyzed an example of a carbonate delta drift previously identified in seismics in order to provide a catalogue of characteristic features at core and sei...
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crwiley:10.1111/sed.12575 2024-09-15T18:31:05+00:00 Facies and sedimentology of a carbonate delta drift (Miocene, Maldives) Reolid, Jesús Betzler, Christian Lüdmann, Thomas Eberli, Gregor Ministerio de Economía y Competitividad Deutsche Forschungsgemeinschaft 2019 http://dx.doi.org/10.1111/sed.12575 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fsed.12575 https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12575 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/sed.12575 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Sedimentology volume 66, issue 4, page 1243-1265 ISSN 0037-0746 1365-3091 journal-article 2019 crwiley https://doi.org/10.1111/sed.12575 2024-08-27T04:32:32Z Abstract The identification of sediment drifts typically relies on interpretation of reflection seismic data sets. This study sedimentologically analyzed an example of a carbonate delta drift previously identified in seismics in order to provide a catalogue of characteristic features at core and seismic scale for allowing testing the occurrence of this poorly known type of deposit elsewhere. Cores and downhole logs recovered during International Ocean Discovery Program Expedition 359 to the Maldives, in combination with seismic data, were analyzed with this objective. The diagnostic criteria for the sedimentological recognition of a delta drift are: (i) the development of sigmoidal clinoforms that thin out towards proximal and distal settings; (ii) a proximal part characterized by coarse‐grained facies with abundant shallow‐water components and distal areas dominated by fine‐grained facies with rare to absent shallow‐water components; (iii) winnowing of the finer fraction in proximal facies; (iv) extensive fragmentation of most of the bioclasts with minor intervals of well‐preserved components; (v) bigradational intervals in the proximal part and large channels in proximal to distal settings; and (vi) the lobe to delta shaped outline of the sediment accumulation. The characteristic shallow‐water fossil assemblage of the Mid to Upper Miocene delta drift consists of large benthic foraminifera ( Amphistegina , Cycloclypeus , Lepidocyclina , Operculina and Heterostegina ), fragmented red algae and bryozoans, equinoid debris, and Halimeda plates. The deeper‐water part of the drift bodies consists of fine‐grained planktonic foraminifera‐rich wackestone. Condensed intervals may occur as result of enhanced bottom‐current activity. In contrast to siliciclastic drift bodies, the carbonate delta drift has an important contribution by in situ shallow‐water carbonate production reminiscent of a shoal. In situ carbonate production is proposed as a major controlling factor which is as important as the pelagic settling or the ... Article in Journal/Newspaper Planktonic foraminifera Wiley Online Library Sedimentology 66 4 1243 1265 |
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Wiley Online Library |
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crwiley |
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English |
description |
Abstract The identification of sediment drifts typically relies on interpretation of reflection seismic data sets. This study sedimentologically analyzed an example of a carbonate delta drift previously identified in seismics in order to provide a catalogue of characteristic features at core and seismic scale for allowing testing the occurrence of this poorly known type of deposit elsewhere. Cores and downhole logs recovered during International Ocean Discovery Program Expedition 359 to the Maldives, in combination with seismic data, were analyzed with this objective. The diagnostic criteria for the sedimentological recognition of a delta drift are: (i) the development of sigmoidal clinoforms that thin out towards proximal and distal settings; (ii) a proximal part characterized by coarse‐grained facies with abundant shallow‐water components and distal areas dominated by fine‐grained facies with rare to absent shallow‐water components; (iii) winnowing of the finer fraction in proximal facies; (iv) extensive fragmentation of most of the bioclasts with minor intervals of well‐preserved components; (v) bigradational intervals in the proximal part and large channels in proximal to distal settings; and (vi) the lobe to delta shaped outline of the sediment accumulation. The characteristic shallow‐water fossil assemblage of the Mid to Upper Miocene delta drift consists of large benthic foraminifera ( Amphistegina , Cycloclypeus , Lepidocyclina , Operculina and Heterostegina ), fragmented red algae and bryozoans, equinoid debris, and Halimeda plates. The deeper‐water part of the drift bodies consists of fine‐grained planktonic foraminifera‐rich wackestone. Condensed intervals may occur as result of enhanced bottom‐current activity. In contrast to siliciclastic drift bodies, the carbonate delta drift has an important contribution by in situ shallow‐water carbonate production reminiscent of a shoal. In situ carbonate production is proposed as a major controlling factor which is as important as the pelagic settling or the ... |
author2 |
Eberli, Gregor Ministerio de Economía y Competitividad Deutsche Forschungsgemeinschaft |
format |
Article in Journal/Newspaper |
author |
Reolid, Jesús Betzler, Christian Lüdmann, Thomas |
spellingShingle |
Reolid, Jesús Betzler, Christian Lüdmann, Thomas Facies and sedimentology of a carbonate delta drift (Miocene, Maldives) |
author_facet |
Reolid, Jesús Betzler, Christian Lüdmann, Thomas |
author_sort |
Reolid, Jesús |
title |
Facies and sedimentology of a carbonate delta drift (Miocene, Maldives) |
title_short |
Facies and sedimentology of a carbonate delta drift (Miocene, Maldives) |
title_full |
Facies and sedimentology of a carbonate delta drift (Miocene, Maldives) |
title_fullStr |
Facies and sedimentology of a carbonate delta drift (Miocene, Maldives) |
title_full_unstemmed |
Facies and sedimentology of a carbonate delta drift (Miocene, Maldives) |
title_sort |
facies and sedimentology of a carbonate delta drift (miocene, maldives) |
publisher |
Wiley |
publishDate |
2019 |
url |
http://dx.doi.org/10.1111/sed.12575 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fsed.12575 https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12575 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/sed.12575 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Sedimentology volume 66, issue 4, page 1243-1265 ISSN 0037-0746 1365-3091 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/sed.12575 |
container_title |
Sedimentology |
container_volume |
66 |
container_issue |
4 |
container_start_page |
1243 |
op_container_end_page |
1265 |
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1810472686508310528 |