Sea level changes versus hydrothermal diagenesis: Origin of Triassic carbonate platform cycles in the Dolomites, Italy-Reference-Cited by-同舟云学术

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Sea level changes versus hydrothermal diagenesis: Origin of Triassic carbonate platform cycles in the Dolomites, Italy

Published:2005-07 Issue:1-2 Volume:178 Page:151-153
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Blendinger W.

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference12 articles.

1. Storm depositional systems;Aigner,1985

2. The carbonate factory of Middle Triassic build-ups of the Dolomites Italy: a quantitative analysis (reply);Blendinger;Sedimentology,1996

3. Sea level changes versus hydrothermal diagenesis: origin of Triassic carbonate platform cycles in the Dolomites, Italy;Blendinger;Sediment. Geol.,2004

4. Geology of the Dolomites—an introduction;Bosellini,1991

5. Facies architecture of an isolated carbonate platform: tracing the cycles of the Latemar (Middle Triassic, northern Italy);Egenhoff;Sedimentology,1999

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Triassic Latemar cycle tops — Subaerial exposure of platform carbonates under tropical arid climate;Sedimentary Geology;2012-07

2. The Allocyclic Interpretation of the ‘Latemar Cycles’ (Middle Triassic, the Dolomites, Italy) and Implications for High-Frequency Cyclostratigraphic Forcing;Perspectives in Carbonate Geology;2012-04-10

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