Titlebook: Studies of Cave Sediments; Physical and Chemica Ira D. Sasowsky,John Mylroie Book 2007 Springer Science+Business Media B.V. 2007 Cave sedim

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Book 2007diverse. They include secondary minerals such as calcite and gypsum, which occur in sundry forms, as well as allogenic and autogenic clasts. This book is for any geoscience researcher or student with interests in climate change, paleohydrology, karst geology, and sedimentology. Studies of Cave Sedim

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Provenance Of Suspended Sediment Discharged From A Karst Aquifer Determined By Clay Mineralogy,t aquifer. Water from Bartom Springs is a significant component of the water resource of Austin, the 21st largest city in the United States. Barton Springs is also a heavily used recreational spot, and it is the sole home of the Barton Springs Salamander (.), an endangered species that is extremely

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,Influence Of Depositional Environment On Devil’s Hole Calcite Morphology And Petrology,that contain at least two different paleoclimate records. Below water table deposits contain a 560,000 year paleoclimate isotopic record (Winograd et al., 1992), while above water table deposists record 120,000 years of changing water tabl elevation (Szabo et al., 1994).

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,Isotope Stage 11, The ‘Super-Interglacial’, From A North Norwegian Speleothem,rctic Circle, is dated by nine TIMS U-series dates to isotope stages 13 and 11. The dates are in perfect stratigraphic order, putting the main growth periods of the speleothem at 502 ka, and 380- 420 ka. Termination V occurred shortly before 421 ±10 ka, probably between 423 and 430 ka, an estimate t

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