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- W1569386690 abstract "The transpressional, intermontane North Park Basin, Colorado, provides excellent examples of sandrich Gilbert-type deltas that prograded into freshwater lacustrine environments. Gilbert-type deltaic sandstones are present in the coal-bearing Palaeocene and Eocene Coalmont Formation. Two types of Gilbert-type sandstone facies are recognized based on their site of deposition, sedimentological properties and nature of the facies of contributing fluvial systems. The transverse Gilbert-type deltaic facies is formed along the basin margin and is composed of vertically stacked sandstone with foreset beds that are thin, slightly variable in thickness and steeply dipping. Multilateral, conglomeratic channel sandstones are formed landward of this deltaic sandstone facies. The longitudinal Gilbert-type deltaic facies is developed in the basin centre and consists of overlapped sandstone bodies with foreset beds that are thick, highly variable in thickness, gently dipping, and interbedded with silty interforesets. The longitudinal deltaic sandstone facies passes upslope into syndepositional growth faults and into multistorey, en echelon fluvial channel sandstones. The transverse, Gilbert-type deltaic sandstone facies was deposited in a rapidly subsiding shallow basin fed by bedload of braided streams. The longitudinal, Gilbert-type deltaic sandstone facies was deposited in a slowly subsiding deep basin, fed by a mixed load or meandering streams. Here, slope-producing, syndepositional growth faults controlled accretion and thickness of the foreset beds." @default.
- W1569386690 created "2016-06-24" @default.
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- W1569386690 date "1990-10-19" @default.
- W1569386690 modified "2023-09-23" @default.
- W1569386690 title "Transverse and Longitudinal Gilbert-Type Deltas, Tertiary Coalmont Formation, North Park Basin, Colorado, USA" @default.
- W1569386690 doi "https://doi.org/10.1002/9781444303858.ch12" @default.
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