: Geology of Petroleum.: Near Fine in Very Good DJ: The Book shows the former owner’s rubberstamped address at the upper corner of the rear . Levorsen, A.I. () Geology of Petroleum. 2nd Edition, W. H. Freeman and Company, San Franciso, CA. It honors the memory of a truly great scientist, petroleum geologist, and teacher. Levorsen’s Geology of Petroleum is a classic; a model. By A.I. Levorsen.

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Geology of Petroleum

International Journal of GeosciencesVol. In the Malita Graben depocentre, the Petrel Frigate and the Echuca Shoals formations source rocks were a poor-to-very good hydrocarbon generating potential, and had attained wet gas window at the present day. Reservoir Traps — General and Structural Doi:. These areas are located respectively km and km northwest of Darwin in the northern Bonaparte Basin, Australia.

Geology of Petroleum by A.I. Levorsen –

This site uses cookies. The traps in the Sahul Platform have been effective to receive the migrated hydrocarbon.

American Association of Petroleum Geologists. It covers the petrkleum of reservoirs, including reservoir rock, pore space, fluids, traps, and mechanics, as well as describing the origin of petroleum and the migration and accumulation of petroleum.

By continuing to use our website, you are agreeing to our privacy policy. The Flamingo, and the Echuca Shoals formations source rocks in the same field were a fair and good hydrocarbon generation potential respectively, and both reached mid-mature oil window.


Reservoir Conditions — Pressure and Temperature Doi:. Migration and Accumulation of Petroleum Doi:. Based on the structural evolution of the northern Bonaparte Basin, data from the wells Loxton Shoals 1, Sunset 1 and Chuditch 1 in the Sahul Platform and Heron 1 in the Malita Graben depocentre, and the Seismic Line N were used to clarify the geological conditions and reconstruct the hydrocarbon accumulation processes in the study area.

Geology of Petroleum A. The Plover, Petrel Frigate and Echuca Shoals formations source rocks in the wells Chuditch 1 and Heron 1, except for the Flamingo Formation in the well Chuditch 1, had higher gas and oil expelling efficiencies than the Plover Formation source rock of the wells in the Sunset-Loxton Shoals field.

Citing Books via Google Scholar. American Association of Petroleum Geologists Foundation. BasinMod 1-D, 2-D, and 3-D software was used for modeling. Scientific Research An Academic Publisher.

W h ither the Full Season: A commemorative edition reprint of the classic volume originally published inthis book remains a useful reference resource for working petroleum geologists as well as students. The Middle Jurassic Plover Formation sandstone reservoir in the Sunset-Loxton field was a poor-to-very good quality and potential for gas beds, petroleeum it was a very poor-to-very good quality and potential for gas beds in the Chuditch field. The Geologic History of Petroleum.


The Petroleum Prospect Doi:. The Petroleum Province Doi:.

The Reservoir Pore Space Doi:. Introduction and Summary Doi:.

Reservoir Traps continued — Stratigraphic and Fluid Doi:. American Association of Petroleum Geologists Published: The Origin of Petroleum Doi:. Nowadays, the main migration pathways are from the southeastward and southward of the Sunset-Loxton Shoals field, and from southward and eastward of the Chuditch field, precisely from the hydrocarbon source kitchens of the Malita Graben depocentre.

The intensities of gas generation and expulsion were more than of peroleum ones either in the Sahul Platform or in the Malita Graben. The Occurrence of Petroleum Doi:. Read more Read less. Sign In or Create an Account. The Plover Formation source rock was a poor-to-good hydrocarbon generative potential and reached the middle to late mature oil window in the Sunset-Loxton Shoals field whereas in the Chuditch field, it was an overall fair-to-good hydrocarbon generative potential, and attained the Late mature oil window.

The Reservoir Rock Doi:.

In the Chuditch field, the hydrocarbon migration to the Plover Formation sandstone reservoir was initiated during the Late Miocene at 7.