Pinch-out style and position of tidally influenced strata in a regressive-transgressive wave-dominated deltaic sandbody, Twentymile Sandstone, Mesaverde Group, NW Colorado-Reference-Cited by-同舟云学术

Pinch-out style and position of tidally influenced strata in a regressive-transgressive wave-dominated deltaic sandbody, Twentymile Sandstone, Mesaverde Group, NW Colorado

Published:2001-04-06 Issue:2 Volume:48 Page:399-414
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Seidler Lars,Steel Ron

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1046/j.1365-3091.2001.00370.x/fullpdf

Reference35 articles.

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2. 2T. Benda (2000 )Architecture, facies and sequence stratigraphy of a fourth order clastic wedge, Twentymile Sandstone (Mesaverde Group), north-west Colorado.Unpublished MSc Thesis, University of Wyoming.

3. 3T. Benda, and R.J. Steel (2000 ) Architecture, facies, and sequence stratigraphy of a fourth-order clastic wedge; Twentymile Sandstone, Mesaverde Group, NW Colorado . In:AAPG 2000 Annual Meeting Abstracts, A12.

4. 4J.P. Bhattacharya, and R.G. Walker (1992 ) Deltas . In:Facies Models - Response to Sea Level Change(Eds R.G. Walker and N.P. James), pp. 155-177. Geological Association of Canada, St Johns, Canada.

5. 5R.G. Bromley (1996 )Trace Fossils, 2nd edn. Chapman & Hall, London, 361 pp.

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