FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2140585280> ?p ?o ?g. }

• W2140585280 abstract "Abstract Upper Triassic strata in the Trutch (94 G) NTS map area consist of the Charlie Lake, Baldonnel and Pardonet formations. These units comprise a mixed siliciclastic-carbonate succession, approximately 350 to 400 m thick. Sediments accumulated along a low gradient continental ramp deposited on the northwestern margin of Pangaea. Twenty-two lithofacies, deposited in distal offshore through supratidal settings are documented. Seven recurrent facies associations are identified in these strata; four reflecting deposition in continental to marginal marine settings, and three reflecting shallow to deep water marine deposition. Facies association 1 (FA1) consists of interbedded dolomitic mudstone/siltstone and dolomitic sandstone that was deposited in an intertidal flat depositional setting. Facies association 2 (FA2) consists of normally graded, trough cross-bedded to current ripple-laminated lenticular beds of mudclast-rich fine- to medium-grained sandstone, and was deposited by a series of small tidal channels. Facies association 3 (FA3) consists of well-sorted fine-grained sandstone beds characterized by high-angle tabular to wedge-shaped cross-beds, low-angle planar cross-beds, low-relief, translatent ripples and inversely graded lamina sets. FA3 is interpreted to represent deposition by a series of elongate, shore-parallel aeolian dunes. Facies association 4 (FA4) consists of a heterogeneous succession of solution collapse breccias, rooted, pedogenically-altered mudstone and siltstone, and wave-rippled very fine- to fine-grained sandstone. It is interpreted as ephemeral lacustrine and/or supratidal sabkha. Facies association 5 (FA5) consists of variably bioclastic quartzose sandstone, crinoidal packstone-grainstone and bivalve-dominated packstone beds. It is interpreted as a wave-dominated shoreface to foreshore on a shallow (inner) ramp. Facies association 6 (FA6) is dominated by very fine-grained calcareous sandstone and thin to thick-bedded bivalve-dominated wackestone, packstone and grainstone. It is interpreted as medial ramp (i.e., offshore transition to proximal offshore). Facies association 7 (FA7) consists primarily of organic-rich calcareous siltstone and mudstone (commonly with abundant carbonate concretions) and variably thick tightly packed bivalve packstone/grainstone beds. It is interpreted as outer ramp (proximal to distal offshore). Siliciclastic sediment in the study area was derived from a variety of sources, including fluvial input from the east-northeast, longshore drift from the north, and aeolian input sourced from marginal marine dune fields. Carbonate sediment in the study interval consists primarily of bioclastic detritus, although non-skeletal grains, particularly faecal pellets, and ooids are locally common. Skeletal carbonate material is dominated by disarticulated mollusc valves and crinoid skeletal debris but also includes ammonoids, articulate brachiopods, gastropods. Vertebrates (fish and reptiles) are also common." @default.
• W2140585280 created "2016-06-24" @default.
• W2140585280 creator A5010976769 @default.
• W2140585280 date "2004-12-01" @default.
• W2140585280 modified "2023-09-26" @default.
• W2140585280 title "Sedimentology of the Upper Triassic Charlie Lake, Baldonnel and Pardonet formations from outcrop exposures in the southern Trutch region, northeastern British Columbia" @default.
• W2140585280 cites W101633874 @default.
• W2140585280 cites W1516513688 @default.
• W2140585280 cites W153007483 @default.
• W2140585280 cites W1533729466 @default.
• W2140585280 cites W1565132727 @default.
• W2140585280 cites W1579735705 @default.
• W2140585280 cites W1580326543 @default.
• W2140585280 cites W1757525421 @default.
• W2140585280 cites W1917585939 @default.
• W2140585280 cites W1921761581 @default.
• W2140585280 cites W1965019247 @default.
• W2140585280 cites W1971696482 @default.
• W2140585280 cites W1972818400 @default.
• W2140585280 cites W1974852401 @default.
• W2140585280 cites W1975920040 @default.
• W2140585280 cites W1979563841 @default.
• W2140585280 cites W1987126212 @default.
• W2140585280 cites W1997687982 @default.
• W2140585280 cites W2008521780 @default.
• W2140585280 cites W2009438605 @default.
• W2140585280 cites W2009655626 @default.
• W2140585280 cites W2037653760 @default.
• W2140585280 cites W2044483107 @default.
• W2140585280 cites W2049379984 @default.
• W2140585280 cites W2049452585 @default.
• W2140585280 cites W2052346014 @default.
• W2140585280 cites W2055496354 @default.
• W2140585280 cites W2058391377 @default.
• W2140585280 cites W2058727796 @default.
• W2140585280 cites W2061526312 @default.
• W2140585280 cites W2063857931 @default.
• W2140585280 cites W2067788615 @default.
• W2140585280 cites W2067948719 @default.
• W2140585280 cites W2069667345 @default.
• W2140585280 cites W2070290398 @default.
• W2140585280 cites W2070595721 @default.
• W2140585280 cites W2074853666 @default.
• W2140585280 cites W2083427109 @default.
• W2140585280 cites W2098757316 @default.
• W2140585280 cites W2099284986 @default.
• W2140585280 cites W2108511223 @default.
• W2140585280 cites W2109178298 @default.
• W2140585280 cites W2109899354 @default.
• W2140585280 cites W2113074837 @default.
• W2140585280 cites W2116680037 @default.
• W2140585280 cites W2116746775 @default.
• W2140585280 cites W2117470562 @default.
• W2140585280 cites W2118660453 @default.
• W2140585280 cites W2123591442 @default.
• W2140585280 cites W2126849800 @default.
• W2140585280 cites W2132907539 @default.
• W2140585280 cites W2133421736 @default.
• W2140585280 cites W2143751596 @default.
• W2140585280 cites W2152773897 @default.
• W2140585280 cites W2157695151 @default.
• W2140585280 cites W2161302974 @default.
• W2140585280 cites W2163191056 @default.
• W2140585280 cites W2210899932 @default.
• W2140585280 cites W2265432222 @default.
• W2140585280 cites W2316624513 @default.
• W2140585280 cites W2495959640 @default.
• W2140585280 cites W2565798416 @default.
• W2140585280 cites W2802765788 @default.
• W2140585280 cites W2900293603 @default.
• W2140585280 cites W2908724520 @default.
• W2140585280 cites W2909005005 @default.
• W2140585280 cites W2909343715 @default.
• W2140585280 cites W2909545348 @default.
• W2140585280 cites W2909798853 @default.
• W2140585280 cites W2910041393 @default.
• W2140585280 cites W2910340998 @default.
• W2140585280 cites W2910371324 @default.
• W2140585280 cites W2910543852 @default.
• W2140585280 cites W2910967724 @default.
• W2140585280 cites W2911046268 @default.
• W2140585280 cites W2911090174 @default.
• W2140585280 cites W399737420 @default.
• W2140585280 cites W621074636 @default.
• W2140585280 doi "https://doi.org/10.2113/52.4.343" @default.
• W2140585280 hasPublicationYear "2004" @default.
• W2140585280 type Work @default.
• W2140585280 sameAs 2140585280 @default.
• W2140585280 citedByCount "12" @default.
• W2140585280 countsByYear W21405852802012 @default.
• W2140585280 countsByYear W21405852802013 @default.
• W2140585280 countsByYear W21405852802015 @default.
• W2140585280 countsByYear W21405852802016 @default.
• W2140585280 countsByYear W21405852802019 @default.
• W2140585280 crossrefType "journal-article" @default.
• W2140585280 hasAuthorship W2140585280A5010976769 @default.
• W2140585280 hasConcept C104873425 @default.
• W2140585280 hasConcept C109007969 @default.
• W2140585280 hasConcept C114793014 @default.
• W2140585280 hasConcept C126753816 @default.

• next