Hildebrand robert s (3 risultati)
Lingua: Inglese
Editore: Econ Geol, 1986
- Brossura
- Rivista/periodico
Da: Larry W Price Books, Portland, OR, U.S.A.Larry W Price Books
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Molto buono
EUR 7,85
EUR 4,24 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Aggiungi al carrelloPamphlet. Condizione: Very Good. Vol 81, pp. 640-659, Maps, Illus, 4to, Extracted from orig Vol, begins with title page, trimmed & stapled, thus is like a pamphlet, last page in facsimile, else VG.
- Brossura
Da: Libereso, Amsterdam, Paesi BassiLibereso
Contatta il venditoreVenditore con 5 stelleCondizione: Usato
EUR 61,90
EUR 50,00 spedizioneSpedito da Paesi Bassi a U.S.A.Quantità: 1 disponibili
Softcover. Incl map. Almost as new. Unread. 169 pp.
The tectonic setting and origin of cretaceous batholiths within the North American cordillera : the case for slab failure magmatism and its significance for crustal growth
edited by Robert S. Hildebrand, Joseph B. Whalen, Geological Survey of Canada
Lingua: Inglese
Editore: Boulder, Colorado : The Geological Society of America, 2017
- Brossura
Da: Joseph Burridge Books, Dagenham, Regno UnitoJoseph Burridge Books
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 132,44
EUR 31,56 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Soft cover. Condizione: New. iv, 133 pages : colour illustrations ; 28 cm. + 1 map. In this Special Paper, Hildebrand and Whalen present a big-picture, paradigm-busting synthesis that examines the tectonic setting, temporal relations, and geochemistry of many plutons within Cretaceous batholithic terranes of the North American C…ordillera. In addition to their compelling tectonic synthesis, they argue that most of the batholiths are not products of arc magmatism as commonly believed, but instead were formed by slab failure during and after collision. They show that slab window and Precambrian TTG suites share many geochemical similarities with Cretaceous slab failure rocks. Geochemical and isotopic data indicate that the slab failure magmas were derived dominantly from the mantle and thus have been one of the largest contributors to growth of continental crust. The authors also note that slab failure plutons emplaced into the epizone are commonly associated with Cu-Au porphyries, as well as Li-Cs-Ta pegmatites.
