Microfacies of carbonate slope boulders: Indicator of the source area (Middle triassic: Mahlknecht cliff, western Dolomites)

Author:

Brandner Rainer,Flügel Erik,Senowbari-Daryan Baba

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Stratigraphy,Geology

Reference63 articles.

1. Biddle, K.T. (1979): Characteristics of Triassic carbonate buildups, Dolomite Alps, Italy: evidence from the margin-to-basin depositional system.—Diss. Rice Univ., 216 p., Houston

2. — (1981): The basal Cipit boulders: Indicators of Middle to Upper Triassic buildup margins, Dolomite Alps, Italy.—Riv. Ital. Palaeont. Strat.,86, 779–794, Milano

3. — (1984): Triassic sea-level change and the Ladinian-Carnian stage boundary.—Nature,308, No. 5960, 631–633, 2 Figs., London

4. Buczynski, C. &Chafetz, H.S. (1991): Habit of bacterially induced precipitates of calcium carbonate and the influence of medium viscosity on mineralogy.—J. Sed. Petrol.,61/2, 226–233, 3 Figs., Tulsa

5. Blendinger, W. &Blendinger, E. (1989): Windward-leewardeffect on Triassic carbonate bank margin facies of the Dolomites, northern Italy.—Sed. Geol.,64, 143–166, 18 Figs., Amsterdam

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