Neogene evolution of the Himalayan-Tibetan region: constraints from ODP site 758, northern ninetyeast ridge; bearing on climatic change
- 1 August 1992
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 95 (1-2) , 95-110
- https://doi.org/10.1016/0031-0182(92)90167-4
Abstract
No abstract availableKeywords
This publication has 67 references indexed in Scilit:
- Neogene tectonics in the Western Mediterranean may have caused the Messinian salinity crisis and an associated glacial eventPublished by Elsevier ,2003
- Stress‐induced changes in plate density, vail sequences, epeirogeny, and short‐lived global sea level fluctuationsTectonics, 1991
- The contact between the Higher Himalaya Crystallines and the Tibetan Sedimentary Series: Miocene large‐scale dextral shearingTectonics, 1991
- An important current reversal (influx) in the Rifian Corridor (Morocco) at the Tortonian‐Messinian boundary: The end of Tethys OceanPaleoceanography and Paleoclimatology, 1991
- Late Neogene paleoceanography and paleoclimatology of the Gulf of Aden region based on calcareous nannofossilsPaleoceanography and Paleoclimatology, 1990
- Miocene deepwater oceanographyPaleoceanography and Paleoclimatology, 1989
- Change from Late Tertiary compression to Quaternary extension in southern Tibet during the India‐Asia CollisionTectonics, 1987
- The Magnetic Epoch-6 carbon shift: A change in the ocean's 13C/12C ratio 6.2 million years agoMarine Micropaleontology, 1980
- Global magmatic episodes: New evidence and implications for the steady-state mid-oceanic ridgeGeology, 1979
- The terminal Miocene eventMarine Micropaleontology, 1976