Coupled ‘storm‐flood’ depositional model: Application to the Miocene–Modern Baram Delta Province, north‐west Borneo
The Miocene to Modern Baram Delta Province is a highly efficient source to sink system that has accumulated 9 to 12 km of coastal–deltaic to shelf sediments over the past 15 Myr. Facies analysis based on ca 1 km of total vertical outcrop stratigraphy, combined with subsurface geology and sedimentary...
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| creator | Collins, Daniel S. Johnson, Howard D. Allison, Peter A. Guilpain, Pierre Damit, Abdul Razak Marzo, Mariano |
| description | The Miocene to Modern Baram Delta Province is a highly efficient source to sink system that has accumulated 9 to 12 km of coastal–deltaic to shelf sediments over the past 15 Myr. Facies analysis based on ca 1 km of total vertical outcrop stratigraphy, combined with subsurface geology and sedimentary processes in the present‐day Baram Delta Province, suggests a ‘storm‐flood’ depositional model comprising two distinct periods: (i) fair‐weather periods are dominated by alongshore sediment reworking and coastal sand accumulation; and (ii) monsoon‐driven storm periods are characterized by increased wave‐energy and offshore‐directed downwelling storm flow that occur simultaneously with peak fluvial discharge caused by storm precipitation (‘storm‐floods’). The modern equivalent environment has the following characteristics: (i) humid‐tropical monsoonal climate; (ii) narrow (ca |
| doi_str_mv | 10.1111/sed.12316 |
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Facies analysis based on ca 1 km of total vertical outcrop stratigraphy, combined with subsurface geology and sedimentary processes in the present‐day Baram Delta Province, suggests a ‘storm‐flood’ depositional model comprising two distinct periods: (i) fair‐weather periods are dominated by alongshore sediment reworking and coastal sand accumulation; and (ii) monsoon‐driven storm periods are characterized by increased wave‐energy and offshore‐directed downwelling storm flow that occur simultaneously with peak fluvial discharge caused by storm precipitation (‘storm‐floods’). The modern equivalent environment has the following characteristics: (i) humid‐tropical monsoonal climate; (ii) narrow (ca <100 km) and steep (ca 1°), densely vegetated, coastal plain; (iii) deep tropical weathering of a mudstone‐dominated hinterland; (iv) multiple independent, small to moderate‐sized (102 to 105 km2) drainage basins; (v) predominance of river‐mouth bypassing; and (vi) supply‐dominated shelf. The ancient, proximal part of this system (the onshore Belait Formation) is dominated by strongly cyclical sandier‐upward successions (metre to decametre‐scale) comprising (from bottom to top): (i) finely laminated mudstone with millimetre‐scale silty laminae; (ii) heterolithic sandstone–mudstone alternations (centimetre to metre‐scale); and (iii) sharp‐based, swaley cross‐stratified sandstone beds and bedsets (metre to decimetre‐scale). Gutter casts (decimetre to metre‐scale) are widespread, they are filled with swaley cross‐stratified sandstone and their long axes are oriented perpendicular to the palaeo‐shoreline. The gutter casts and other associated waning‐flow event beds suggest that erosion and deposition was controlled by high‐energy, offshore‐directed, oscillatory‐dominated, sediment‐laden combined flows within a shoreface to delta front setting. The presence of multiple river mouths and exceptionally high rates of accommodation creation (characteristic of the Neogene to Recent Baram Delta Province; up to 3000 m Ma−1), in a ‘storm‐flood’‐dominated environment, resulted in a highly efficient and effective offshore‐directed sediment transport system.</description><identifier>ISSN: 0037-0746</identifier><identifier>EISSN: 1365-3091</identifier><identifier>DOI: 10.1111/sed.12316</identifier><language>eng</language><publisher>Madrid: Wiley Subscription Services, Inc</publisher><subject>Accommodation ; Accumulation ; Alternations ; Axes (reference lines) ; Baram Delta Province ; Basins ; Casts ; Climate ; Climatology ; Coastal plains ; Coastal zone management ; Coasts ; combined flow ; delta front ; Discharge ; Downwelling ; Drainage ; Drainage basins ; Energy ; Erosion ; Erosion control ; Facies ; Floods ; Geology ; gutter cast ; humid‐tropical ; Laminates ; Miocene ; Mudstone ; Neogene ; Offshore ; Outcrops ; Paleoshorelines ; Precipitation ; River basins ; River mouth ; Rivers ; Sandstone ; Sediment ; Sediment transport ; Sedimentary rocks ; Sediments ; shoreface ; Shorelines ; Storms ; storm‐flood ; Stratigraphy ; Transport ; Weather ; Weathering</subject><ispartof>Sedimentology, 2017-08, Vol.64 (5), p.1203-1235</ispartof><rights>2016 The Authors. published by John Wiley & Sons Ltd on behalf of International Association of Sedimentologists.</rights><rights>Journal compilation © 2017 International Association of Sedimentologists</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4216-3b296e74ed8026d323aa78432919f265722c486be59367902d3f76417b154c403</citedby><cites>FETCH-LOGICAL-a4216-3b296e74ed8026d323aa78432919f265722c486be59367902d3f76417b154c403</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fsed.12316$$EPDF$$P50$$Gwiley$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fsed.12316$$EHTML$$P50$$Gwiley$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids></links><search><creatorcontrib>Collins, Daniel S.</creatorcontrib><creatorcontrib>Johnson, Howard D.</creatorcontrib><creatorcontrib>Allison, Peter A.</creatorcontrib><creatorcontrib>Guilpain, Pierre</creatorcontrib><creatorcontrib>Damit, Abdul Razak</creatorcontrib><creatorcontrib>Marzo, Mariano</creatorcontrib><title>Coupled ‘storm‐flood’ depositional model: Application to the Miocene–Modern Baram Delta Province, north‐west Borneo</title><title>Sedimentology</title><description>The Miocene to Modern Baram Delta Province is a highly efficient source to sink system that has accumulated 9 to 12 km of coastal–deltaic to shelf sediments over the past 15 Myr. Facies analysis based on ca 1 km of total vertical outcrop stratigraphy, combined with subsurface geology and sedimentary processes in the present‐day Baram Delta Province, suggests a ‘storm‐flood’ depositional model comprising two distinct periods: (i) fair‐weather periods are dominated by alongshore sediment reworking and coastal sand accumulation; and (ii) monsoon‐driven storm periods are characterized by increased wave‐energy and offshore‐directed downwelling storm flow that occur simultaneously with peak fluvial discharge caused by storm precipitation (‘storm‐floods’). The modern equivalent environment has the following characteristics: (i) humid‐tropical monsoonal climate; (ii) narrow (ca <100 km) and steep (ca 1°), densely vegetated, coastal plain; (iii) deep tropical weathering of a mudstone‐dominated hinterland; (iv) multiple independent, small to moderate‐sized (102 to 105 km2) drainage basins; (v) predominance of river‐mouth bypassing; and (vi) supply‐dominated shelf. The ancient, proximal part of this system (the onshore Belait Formation) is dominated by strongly cyclical sandier‐upward successions (metre to decametre‐scale) comprising (from bottom to top): (i) finely laminated mudstone with millimetre‐scale silty laminae; (ii) heterolithic sandstone–mudstone alternations (centimetre to metre‐scale); and (iii) sharp‐based, swaley cross‐stratified sandstone beds and bedsets (metre to decimetre‐scale). Gutter casts (decimetre to metre‐scale) are widespread, they are filled with swaley cross‐stratified sandstone and their long axes are oriented perpendicular to the palaeo‐shoreline. The gutter casts and other associated waning‐flow event beds suggest that erosion and deposition was controlled by high‐energy, offshore‐directed, oscillatory‐dominated, sediment‐laden combined flows within a shoreface to delta front setting. The presence of multiple river mouths and exceptionally high rates of accommodation creation (characteristic of the Neogene to Recent Baram Delta Province; up to 3000 m Ma−1), in a ‘storm‐flood’‐dominated environment, resulted in a highly efficient and effective offshore‐directed sediment transport system.</description><subject>Accommodation</subject><subject>Accumulation</subject><subject>Alternations</subject><subject>Axes (reference lines)</subject><subject>Baram Delta Province</subject><subject>Basins</subject><subject>Casts</subject><subject>Climate</subject><subject>Climatology</subject><subject>Coastal plains</subject><subject>Coastal zone management</subject><subject>Coasts</subject><subject>combined flow</subject><subject>delta front</subject><subject>Discharge</subject><subject>Downwelling</subject><subject>Drainage</subject><subject>Drainage basins</subject><subject>Energy</subject><subject>Erosion</subject><subject>Erosion control</subject><subject>Facies</subject><subject>Floods</subject><subject>Geology</subject><subject>gutter cast</subject><subject>humid‐tropical</subject><subject>Laminates</subject><subject>Miocene</subject><subject>Mudstone</subject><subject>Neogene</subject><subject>Offshore</subject><subject>Outcrops</subject><subject>Paleoshorelines</subject><subject>Precipitation</subject><subject>River basins</subject><subject>River mouth</subject><subject>Rivers</subject><subject>Sandstone</subject><subject>Sediment</subject><subject>Sediment transport</subject><subject>Sedimentary rocks</subject><subject>Sediments</subject><subject>shoreface</subject><subject>Shorelines</subject><subject>Storms</subject><subject>storm‐flood</subject><subject>Stratigraphy</subject><subject>Transport</subject><subject>Weather</subject><subject>Weathering</subject><issn>0037-0746</issn><issn>1365-3091</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNp1kM1Kw0AQxxdRsFYPvsGCJ8G0-5Xdrrd--QEtCuo5bJMJTUmzcTe19CDkEQQv-np9ElPr1bkMDL_5D_ND6JySDm2q6yHpUMapPEAtymUYcKLpIWoRwlVAlJDH6MT7BSFUip5uofehXZU5JHhbf_nKuuW2_khza5Nt_Y0TKK3PqswWJsdLm0B-jftlmWex2Q1xZXE1BzzNbAwFbOvPacO4Ag-MM0s8grwy-NHZt6yI4QoX1lXzJn4NvsID6wqwp-goNbmHs7_eRi834-fhXTB5uL0f9ieBEYzKgM-YlqAEJD3CZMIZN0b1BGea6pTJUDEWi56cQai5VJqwhKdKCqpmNBSxILyNLva5pbOvq-Z-tLAr13zlI6ppyChVRDfU5Z6KnfXeQRqVLlsat4koiXZ2o8Zu9Gu3Ybt7dp3lsPkfjJ7Go_3GD90ff7o</recordid><startdate>201708</startdate><enddate>201708</enddate><creator>Collins, Daniel S.</creator><creator>Johnson, Howard D.</creator><creator>Allison, Peter A.</creator><creator>Guilpain, Pierre</creator><creator>Damit, Abdul Razak</creator><creator>Marzo, Mariano</creator><general>Wiley Subscription Services, Inc</general><scope>24P</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>201708</creationdate><title>Coupled ‘storm‐flood’ depositional model: Application to the Miocene–Modern Baram Delta Province, north‐west Borneo</title><author>Collins, Daniel S. ; Johnson, Howard D. ; Allison, Peter A. ; Guilpain, Pierre ; Damit, Abdul Razak ; Marzo, Mariano</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4216-3b296e74ed8026d323aa78432919f265722c486be59367902d3f76417b154c403</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Accommodation</topic><topic>Accumulation</topic><topic>Alternations</topic><topic>Axes (reference lines)</topic><topic>Baram Delta Province</topic><topic>Basins</topic><topic>Casts</topic><topic>Climate</topic><topic>Climatology</topic><topic>Coastal plains</topic><topic>Coastal zone management</topic><topic>Coasts</topic><topic>combined flow</topic><topic>delta front</topic><topic>Discharge</topic><topic>Downwelling</topic><topic>Drainage</topic><topic>Drainage basins</topic><topic>Energy</topic><topic>Erosion</topic><topic>Erosion control</topic><topic>Facies</topic><topic>Floods</topic><topic>Geology</topic><topic>gutter cast</topic><topic>humid‐tropical</topic><topic>Laminates</topic><topic>Miocene</topic><topic>Mudstone</topic><topic>Neogene</topic><topic>Offshore</topic><topic>Outcrops</topic><topic>Paleoshorelines</topic><topic>Precipitation</topic><topic>River basins</topic><topic>River mouth</topic><topic>Rivers</topic><topic>Sandstone</topic><topic>Sediment</topic><topic>Sediment transport</topic><topic>Sedimentary rocks</topic><topic>Sediments</topic><topic>shoreface</topic><topic>Shorelines</topic><topic>Storms</topic><topic>storm‐flood</topic><topic>Stratigraphy</topic><topic>Transport</topic><topic>Weather</topic><topic>Weathering</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Collins, Daniel S.</creatorcontrib><creatorcontrib>Johnson, Howard D.</creatorcontrib><creatorcontrib>Allison, Peter A.</creatorcontrib><creatorcontrib>Guilpain, Pierre</creatorcontrib><creatorcontrib>Damit, Abdul Razak</creatorcontrib><creatorcontrib>Marzo, Mariano</creatorcontrib><collection>Wiley Online Library Open Access</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</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>Environment Abstracts</collection><jtitle>Sedimentology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Collins, Daniel S.</au><au>Johnson, Howard D.</au><au>Allison, Peter A.</au><au>Guilpain, Pierre</au><au>Damit, Abdul Razak</au><au>Marzo, Mariano</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coupled ‘storm‐flood’ depositional model: Application to the Miocene–Modern Baram Delta Province, north‐west Borneo</atitle><jtitle>Sedimentology</jtitle><date>2017-08</date><risdate>2017</risdate><volume>64</volume><issue>5</issue><spage>1203</spage><epage>1235</epage><pages>1203-1235</pages><issn>0037-0746</issn><eissn>1365-3091</eissn><abstract>The Miocene to Modern Baram Delta Province is a highly efficient source to sink system that has accumulated 9 to 12 km of coastal–deltaic to shelf sediments over the past 15 Myr. Facies analysis based on ca 1 km of total vertical outcrop stratigraphy, combined with subsurface geology and sedimentary processes in the present‐day Baram Delta Province, suggests a ‘storm‐flood’ depositional model comprising two distinct periods: (i) fair‐weather periods are dominated by alongshore sediment reworking and coastal sand accumulation; and (ii) monsoon‐driven storm periods are characterized by increased wave‐energy and offshore‐directed downwelling storm flow that occur simultaneously with peak fluvial discharge caused by storm precipitation (‘storm‐floods’). The modern equivalent environment has the following characteristics: (i) humid‐tropical monsoonal climate; (ii) narrow (ca <100 km) and steep (ca 1°), densely vegetated, coastal plain; (iii) deep tropical weathering of a mudstone‐dominated hinterland; (iv) multiple independent, small to moderate‐sized (102 to 105 km2) drainage basins; (v) predominance of river‐mouth bypassing; and (vi) supply‐dominated shelf. The ancient, proximal part of this system (the onshore Belait Formation) is dominated by strongly cyclical sandier‐upward successions (metre to decametre‐scale) comprising (from bottom to top): (i) finely laminated mudstone with millimetre‐scale silty laminae; (ii) heterolithic sandstone–mudstone alternations (centimetre to metre‐scale); and (iii) sharp‐based, swaley cross‐stratified sandstone beds and bedsets (metre to decimetre‐scale). Gutter casts (decimetre to metre‐scale) are widespread, they are filled with swaley cross‐stratified sandstone and their long axes are oriented perpendicular to the palaeo‐shoreline. The gutter casts and other associated waning‐flow event beds suggest that erosion and deposition was controlled by high‐energy, offshore‐directed, oscillatory‐dominated, sediment‐laden combined flows within a shoreface to delta front setting. The presence of multiple river mouths and exceptionally high rates of accommodation creation (characteristic of the Neogene to Recent Baram Delta Province; up to 3000 m Ma−1), in a ‘storm‐flood’‐dominated environment, resulted in a highly efficient and effective offshore‐directed sediment transport system.</abstract><cop>Madrid</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1111/sed.12316</doi><tpages>33</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Accommodation Accumulation Alternations Axes (reference lines) Baram Delta Province Basins Casts Climate Climatology Coastal plains Coastal zone management Coasts combined flow delta front Discharge Downwelling Drainage Drainage basins Energy Erosion Erosion control Facies Floods Geology gutter cast humid‐tropical Laminates Miocene Mudstone Neogene Offshore Outcrops Paleoshorelines Precipitation River basins River mouth Rivers Sandstone Sediment Sediment transport Sedimentary rocks Sediments shoreface Shorelines Storms storm‐flood Stratigraphy Transport Weather Weathering |
| title | Coupled ‘storm‐flood’ depositional model: Application to the Miocene–Modern Baram Delta Province, north‐west Borneo |
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