Developments in sedimentary provenance studies by A. C. Morton, Seldon P., Jr. Todd, P. D. W. Haughton

By A. C. Morton, Seldon P., Jr. Todd, P. D. W. Haughton

Show description

Read Online or Download Developments in sedimentary provenance studies PDF

Similar geology books

Violet Earth Artbook Альбом с иллюстрациями

Книга Violet Earth Artbook Альбом с иллюстрациями Violet Earth Artbook Альбом с иллюстрациями Книги Искусство. Живопись Автор: Shunya Yamashita Формат: different Размер: sixty three. nine Мб Язык: Русский0 (голосов: zero) Оценка:Shunya Yamashita, родился в 1970 в префектуре Saitama, Япония, один из самых известных японских художников среди любителей азиатского арта.

Field Techniques for Sea Ice Research

Up to one-tenth of the world’s oceans are lined with sea ice, or frozen ocean water, sooner or later in the course of the annual cycle. Sea ice therefore performs a huge, frequently defining, function within the ordinary surroundings and the worldwide weather procedure. This publication is a world examine the alterations in sea ice and the instruments and methods used to degree and checklist these adjustments.

Additional resources for Developments in sedimentary provenance studies

Sample text

POMEROL, C. 8s TOURENQ, J. 1970. Les Mineraux en Grains. Masson et Cie, Paris. POWER, G. M. 1968. Chemical variations in tourmalines from south-west England. Mineralogical Magazine, 36, 1078-1089. PRESS, S. 1986. Detrital spinels from alpinotype source rocks in Middle Devonian sediments of the Rhenish massif. Geologische Rundschau, 75, 333340. SHUKLA, B. 1988. Provenance of Oligocene Lough Neagh Group, Northern Ireland, United K i n g dom (abstract). In: JAMES, D. P. 8s LECKIE, D. A. (eds) Sequences, stratigraphy, sedimentology: surface and subsurface.

Another alternative, the LondonBrabant Massif, is readily ruled out (Fig. 13), as chloritoids of the Ottre area are distinctly different, with very high MnO values (Fransolet 1978). For comparison, Fig. 13 also shows chloritoid anlayses from Lower Eocene sandstones of the Frigg area (northern North Sea), derived from the Shetland region. These have distinctly higher MnO values compared to Bridport Sands chloritoid. As with the spinel group, little detail is available on stability of detrital chloritoid, although North Sea Jurassic sandstones buried in excess of 4 km contain chloritoid grains that lack a n y evidence of corrosion.

Geological Society of America Bulletin, 82, 629-658. VALLONI, R. 1985. Reading provenance from modern marine sands. In: ZUFFA, G. G. ) Provenance of Arenites. NATO-ASI Series 148, D. Reidel, Dordrecht, 309-332. ZUFFA, G. G. 1969. Arenarie e calcari arenacei miocenici di Vetto-Carpineti (Formazione di Bismantova, Appennino settentrionale). Mineralogica et Petrographica Acta, 15, 191-212. 1980. Hybrid arenites: their composition and classification. Journal of Sedimentary Petrology, 50, 21-29. 1985.

Download PDF sample

Rated 4.92 of 5 – based on 30 votes