An accretionary distally steepened ramp at an intrashelf basin margin: an alternative explanation for the Upper Triassic Steinplatte “reef” (Northern Calcareous Alps, Austria)-Reference-Cited by-同舟云学术

An accretionary distally steepened ramp at an intrashelf basin margin: an alternative explanation for the Upper Triassic Steinplatte “reef” (Northern Calcareous Alps, Austria)

Published:1995-03 Issue:3-4 Volume:95 Page:269-286
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Stanton Robert J.,Flügel Erik

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference48 articles.

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2. Limestone depositional sequences on shelves and ramps—modern and ancient;Ahr;Geol. Today,1985

3. Progradation geometries of carbonate platforms: examples from the Triassic of the Dolomites, northern Italy;Bosellini;Sedimentology,1984

4. Dynamics of Tethyan carbonate platforms;Bosellini,1989

5. Microfacies of carbonate slope boulders: indicator of the source area (Middle Triassic: Mahlknecht Cliff, Western Dolomites);Brandner;Facies,1991

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