Matches in SemOpenAlex for { <https://semopenalex.org/work/W2794128328> ?p ?o ?g. }
Showing items 1 to 89 of
89
with 100 items per page.
- W2794128328 abstract "The western ancestral Mississippi shelf-margin delta fed the Bryant Canyon turbidite system in the intraslope basin province of the northwestern Gulf of Mexico (GOM) during the penultimate glacial lowstand of sea level (130–160 year BP). The Bryant Canyon links a chain of 15 fill-and-spill minibasins on the continental slope. On the upper and lower continental slopes, minibasins are narrow (1–3 km), elongate (3–6 km), and follow salt ridges. On the middle slope, minibasins are larger (8–15 km) semicircular basins. Three main depositional facies are recognized based on seismic-facies interpretation: (1) ponded turbidites (T), (2) mass-transport deposits (MTDs), and (3) bypass channelized turbidites (C). Thick, intrabasinal, muddy MTD wedges sourced from high-relief internal walls of the minibasins alternate with and frequently cap externally derived deposits. Tabular extrabasinal MTD deposits originated from shelf-margin delta or canyon-wall failures upslope. The T and MTD facies deposits each make up approximately 40% of basin fill, and the C facies deposits comprise approximately 20%. The T facies deposits form perched lobes at canyon inlets into basins and ponded units on distal sides of basins. Channels in the C facies are similar in width (500–2000 m) and relief (20–100 ms) to channels in productive GOM subsurface minibasins. Syntectonic activity of salt diapirs typically began midway through filling of Bryant Canyon minibasins and then preferentially uplifted northern portions of basin deposits. Local salt-tectonic activity caused greater basin relief and thicker capping MTDs than in subsurface minibasins to the west (e.g., Brazos-Trinity Basin IV) or east (e.g., Mississippi Canyon). Bryant Canyon minibasins provide excellent modern analogs for subsurface Miocene to Pleistocene GOM chains of minibasins because of similar scales and depositional facies. The youngest Bryant T facies deposits and their overlying incised, thick, channel deposits contain the most sand-prone facies and suggest the best potential for petroleum reservoirs in subsurface minibasins." @default.
- W2794128328 created "2018-03-29" @default.
- W2794128328 creator A5041541044 @default.
- W2794128328 creator A5071662919 @default.
- W2794128328 creator A5083574242 @default.
- W2794128328 date "2018-05-01" @default.
- W2794128328 modified "2023-09-22" @default.
- W2794128328 title "Late Pleistocene Bryant Canyon turbidite system: Implications for Gulf of Mexico minibasin petroleum systems" @default.
- W2794128328 cites W119333118 @default.
- W2794128328 cites W1795249777 @default.
- W2794128328 cites W1992416885 @default.
- W2794128328 cites W2058714164 @default.
- W2794128328 cites W2067735465 @default.
- W2794128328 cites W2084567529 @default.
- W2794128328 cites W2106103280 @default.
- W2794128328 cites W2123786602 @default.
- W2794128328 cites W2135369138 @default.
- W2794128328 cites W2158248674 @default.
- W2794128328 cites W2194143925 @default.
- W2794128328 cites W2285479480 @default.
- W2794128328 cites W2326561072 @default.
- W2794128328 cites W2476649593 @default.
- W2794128328 cites W2483583879 @default.
- W2794128328 cites W2488225468 @default.
- W2794128328 cites W2498731013 @default.
- W2794128328 cites W2499792186 @default.
- W2794128328 cites W2501118455 @default.
- W2794128328 cites W2502176454 @default.
- W2794128328 cites W2503851567 @default.
- W2794128328 cites W4206074551 @default.
- W2794128328 cites W4250406741 @default.
- W2794128328 doi "https://doi.org/10.1190/int-2017-0150.1" @default.
- W2794128328 hasPublicationYear "2018" @default.
- W2794128328 type Work @default.
- W2794128328 sameAs 2794128328 @default.
- W2794128328 citedByCount "3" @default.
- W2794128328 countsByYear W27941283282021 @default.
- W2794128328 crossrefType "journal-article" @default.
- W2794128328 hasAuthorship W2794128328A5041541044 @default.
- W2794128328 hasAuthorship W2794128328A5071662919 @default.
- W2794128328 hasAuthorship W2794128328A5083574242 @default.
- W2794128328 hasConcept C111368507 @default.
- W2794128328 hasConcept C114793014 @default.
- W2794128328 hasConcept C127313418 @default.
- W2794128328 hasConcept C151730666 @default.
- W2794128328 hasConcept C157954998 @default.
- W2794128328 hasConcept C2816523 @default.
- W2794128328 hasConcept C2985768699 @default.
- W2794128328 hasConcept C53570757 @default.
- W2794128328 hasConcept C548895740 @default.
- W2794128328 hasConcept C84859931 @default.
- W2794128328 hasConceptScore W2794128328C111368507 @default.
- W2794128328 hasConceptScore W2794128328C114793014 @default.
- W2794128328 hasConceptScore W2794128328C127313418 @default.
- W2794128328 hasConceptScore W2794128328C151730666 @default.
- W2794128328 hasConceptScore W2794128328C157954998 @default.
- W2794128328 hasConceptScore W2794128328C2816523 @default.
- W2794128328 hasConceptScore W2794128328C2985768699 @default.
- W2794128328 hasConceptScore W2794128328C53570757 @default.
- W2794128328 hasConceptScore W2794128328C548895740 @default.
- W2794128328 hasConceptScore W2794128328C84859931 @default.
- W2794128328 hasFunder F4320332183 @default.
- W2794128328 hasLocation W27941283281 @default.
- W2794128328 hasOpenAccess W2794128328 @default.
- W2794128328 hasPrimaryLocation W27941283281 @default.
- W2794128328 hasRelatedWork W119333118 @default.
- W2794128328 hasRelatedWork W1853702506 @default.
- W2794128328 hasRelatedWork W2033092286 @default.
- W2794128328 hasRelatedWork W2148498450 @default.
- W2794128328 hasRelatedWork W2157949990 @default.
- W2794128328 hasRelatedWork W2244972914 @default.
- W2794128328 hasRelatedWork W2273860324 @default.
- W2794128328 hasRelatedWork W2280416567 @default.
- W2794128328 hasRelatedWork W2289847069 @default.
- W2794128328 hasRelatedWork W2313743482 @default.
- W2794128328 hasRelatedWork W2327409284 @default.
- W2794128328 hasRelatedWork W2332022613 @default.
- W2794128328 hasRelatedWork W2482154064 @default.
- W2794128328 hasRelatedWork W2483497029 @default.
- W2794128328 hasRelatedWork W2502176454 @default.
- W2794128328 hasRelatedWork W2506172105 @default.
- W2794128328 hasRelatedWork W2980588072 @default.
- W2794128328 hasRelatedWork W3140768429 @default.
- W2794128328 hasRelatedWork W2144501176 @default.
- W2794128328 hasRelatedWork W3112621968 @default.
- W2794128328 isParatext "false" @default.
- W2794128328 isRetracted "false" @default.
- W2794128328 magId "2794128328" @default.
- W2794128328 workType "article" @default.