Architecture of a 1.38–1.34 Ga granite–rhyolite complex as revealed by geochronology and isotopic and elemental geochemistry of subsurface samples from west Texas, USA

Author:

Barnes Melanie A,Anthony Elizabeth Y,Williams Ian,Asquith George B

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference62 articles.

1. Evidence for late Middle Proterozoic extension in the Precambrian basement beneath the Permian basin;Adams;Tectonics,1995

2. Precambrian basement geology of the Permian Basin region of west Texas and eastern New Mexico: a geophysical perspective;Adams;Am. Assoc. Petrol. Geol. Bull.,1996

3. Episodic rapakivi magmatism due to distal orogenesis: correlation of 1.69–1.50 Ga orogenic and inboard, ‘anorogenic’ events in the Baltic Shield;Åhäll;Geology,2000

4. Amarante, J.F.A., 2001. Characterization of the Proterozoic basement rocks in the Mescalero No. 1 well, Guadalupe County, New Mexico, M.Sc. thesis, New Mexico Tech, Socorro, New Mexico, USA.

5. Proterozoic anorogenic granite plutonism of North America;Anderson;Geol. Soc. Am. Membr.,1983

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