GEOLOGIC TIME AS A PARAMETER IN ORGANIC METAMORPHISM AND VITRINITE REFLECTANCE AS AN ABSOLUTE PALEOGEOTHERMOMETER
- 1 July 1983
- journal article
- Published by Wiley in Journal of Petroleum Geology
- Vol. 6 (1), 5-37
- https://doi.org/10.1111/j.1747-5457.1983.tb00260.x
Abstract
No abstract availableKeywords
This publication has 40 references indexed in Scilit:
- Organic geochemistry of core samples from an ultradeep hot well (300°C, 7 km)Chemical Geology, 1982
- Textures of sandstones and carbonate rocks in the world's deepest wells (in excess of 30,000 ft. or 9.1 km): Anadarko Basin, OklahomaSedimentary Geology, 1981
- THE EVOLUTION OF THE DEAD SEA FLOATING ASPHALT BLOCKS: SIMULATIONS BY PYROLYSISJournal of Petroleum Geology, 1980
- Carbon isotope fractionation during coal pyrolysisFuel, 1978
- Effect of prolonged heating on the optical properties of vitriniteFuel, 1977
- L'evolution thermique de la matière organique des sédiments : applications d'une simulation mathématique. Potentiel pétrolier des bassins sédimentaires de reconstitution de l'histoire thermique des sédimentsRevue de l'Institut Français du Pétrole, 1975
- Programmed-temperature pyrolysis of vitrinites of various rankFuel, 1974
- Thermal Alteration of Clastic Organic Particles as an Indicator of Contact and Burial Metamorphism in Sedimentary RocksProceedings of the Annual Meeting. American Association of Stratigraphic Palynologists, 1971
- Heterogeneous Reactions in Petroleum Genesis and MaturationNature, 1969
- Metamorphism of a LigniteNature, 1962