✦ LIBER ✦

Bahamian carbonate platform development in response to sea-level changes and the closure of the Isthmus of Panama

✍ Scribed by John J. Reijmer; Christian Betzler; Dick Kroon; Ralf Tiedemann; Gregor P. Eberli

Book ID: 106177128
Publisher: Springer
Year: 2001
Tongue: English
Weight: 213 KB
Volume: 91
Category: Article
ISSN: 0016-7835
DOI: 10.1007/s00531-001-0235-x

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Sea level changes versus hydrothermal di

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

✍ W Blendinger 📂 Article 📅 2004 🏛 Elsevier Science 🌐 English ⚖ 906 KB

Sea level changes versus hydrothermal di

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

✍ W. Blendinger 📂 Article 📅 2005 🏛 Elsevier Science 🌐 English ⚖ 684 KB

Sea level changes versus hydrothermal di

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

✍ W. Blendinger 📂 Article 📅 2005 🏛 Elsevier Science 🌐 English ⚖ 80 KB

Sea level changes versus hydrothermal di

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

✍ Nereo Preto; Linda A. Hinnov; Lawrence A. Hardie; Mark T. Harris 📂 Article 📅 2005 🏛 Elsevier Science 🌐 English ⚖ 95 KB

Sea level changes versus hydrothermal di

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

✍ Arndt Peterhänsel; Sven O. Egenhoff 📂 Article 📅 2005 🏛 Elsevier Science 🌐 English ⚖ 105 KB

The response of the water table in coast

The response of the water table in coastal aeolian systems to changes in sea level

✍ G Kocurek; N.I Robinson; J.M Sharp Jr. 📂 Article 📅 2001 🏛 Elsevier Science 🌐 English ⚖ 838 KB

The water table in some aeolian systems is a control on the type and rate of accumulation, and defines the depth to which deflation will occur in the formation of regional bounding surfaces. At the basinal scale over time, the elevation of the water table may be a function of climate, tectonism, and