Zobrazeno 1 - 10
of 33
pro vyhledávání: '"B. R. Frost"'
Publikováno v:
GSA Today. 29
Autor:
Christopher Fanning, Seth C. Kruckenberg, Joseph P. Gonzalez, J.F. McLaughlin, Carol D. Frost, Susan M. Swapp, B. R. Frost
Publikováno v:
Geological Society of America Bulletin. 129:259-280
The scarce remnants of Earth’s earliest history make it challenging to describe the crust-forming processes that operated during that time, and all evidence that survived subsequent tectonism and recycling deserves to be studied closely. We present
Publikováno v:
Journal of Petrology. 51:1831-1847
The formation of peralkaline melts is generally recognized to be related to enrichment of the mantle in sodium or potassium during a metasomatic event that predated magma generation. The wide range in mineral assemblages, mineral compositions, and fl
Autor:
Patricia Fryer, Andrew McCaig, Benoit Ildefonse, Roger Searle, B. R. Frost, James S. Beard, Pavel V. Zinin, Shiv K. Sharma
Publikováno v:
Journal of Petrology
Journal of Petrology, Oxford University Press (OUP), 2009, 50 (3), pp.387-403. ⟨10.1093/petrology/egp004⟩
Journal of Petrology, Oxford University Press (OUP), 2009, 50 (3), pp.387-403. ⟨10.1093/petrology/egp004⟩
International audience; Serpentinization of olivine-rich troctolite from core 227, Integrated Ocean Drilling Program (IODP) Hole U1309D ranges from 10 to 90. Two episodes of serpentinization are recognized. The first, dominant in weakly serpentinized
Publikováno v:
Journal of Metamorphic Geology. 27:3-17
The Broken Hill Pb-Zn deposit, New South Wales Australia, is hosted in granulite facies gneisses of the Southern Curnamona Province (SCP) that have long been known to record a polydeformational and polymetamorphic history. The details of this potenti
Publikováno v:
The UW National Parks Service Research Station Annual Reports. 31:89-92
In previous years of this project, we have developed the hypothesis that the high-pressure granulites exposed in the Moose Basin area of the Teton Range represent evidence of a 2.7 billion yearÂold continent-continent collision. We have described
Publikováno v:
Precambrian Research. 119:45-71
Anorthosite complexes commonly are spatially and temporally associated with A-type granite batholiths, but their genetic relationship, if any, has been difficult to determine. This study focuses on the northern portion of the 1.43–1.44 Ga Sherman b
Publikováno v:
Journal of Petrology. 40:1771-1802
The 1·43 Ga Sherman batholith, southeastern Wyoming, USA, origin that are found throughout the Proterozoic ‘anorogenic’ granite provinces of the southwestern USA, Adirshows extreme A-type petrochemical characteristics compared with other Mid-Pro
Publikováno v:
Tectonics. 13:354-366
The University of Wyoming conducted seismic reflection profiling in the Laramie Mountains of Wyoming to investigate the nature of Precambrian crustal structure and Laramide deformation in the region. Here the imaging of layering in the Laramie Anorth