Oxygen isotope evidence for high-altitude snow in the Laramide Rocky Mountains of North America during the Late Cretaceous and Paleogene
- 1 January 2000
- journal article
- Published by Geological Society of America in Geology
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Oxygen and carbon isotope fractionation in biogenic aragonite: Temperature effectsPublished by Elsevier ,2004
- Controls on the stable isotope composition of seasonal growth bands in aragonitic fresh-water bivalves (unionidae)Geochimica et Cosmochimica Acta, 1999
- Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and CenozoicJournal of Geophysical Research, 1995
- Eocene continental climates and latitudinal temperature gradientsGeology, 1995
- Tectonic, stratigraphic, and sedimentologic significance of a regional discontinuity in the upper Judith River Group (Belly River wedge) of southern Alberta, Saskatchewan, and northern MontanaCanadian Journal of Earth Sciences, 1993
- Tectonic significance of paleobotanically estimated climate and altitude of the late Eocene erosion surface, ColoradoGeology, 1992
- Kinematic history of a foreland uplift from Paleocene synorogenic conglomerate, Beartooth Range, Wyoming and MontanaGSA Bulletin, 1991
- Early Oligocene paleovalleys in southern and central Wyoming: Evidence of high local relief on the late Eocene unconformityGeology, 1990
- Explanations of the tertiary global cooling trendPalaeogeography, Palaeoclimatology, Palaeoecology, 1985
- Post-Cretaceous History of the Mountains of Central Western WyomingThe Journal of Geology, 1915