Zobrazeno 1 - 10
of 79
pro vyhledávání: '"M E, Bickford"'
Autor:
Joseph L. Wooden, Mark D. Schmitz, Aaron M. Satkoski, M. E. Bickford, Scott D. Samson, George D. Kamenov, Paul A. Mueller, Robert L. Bauer
Paleoarchean to Mesoarchean gneisses are exposed in the Minnesota River Valley (MRV) and in northern Michigan, USA. The MRV rocks include a complex of granitic migmatites, schistose to gneissic amphibolite, metagabbro, and paragneisses. The best-know
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5ddf3150e2fe0dc29249247291d806e
https://doi.org/10.1016/b978-0-444-63901-1.00027-7
https://doi.org/10.1016/b978-0-444-63901-1.00027-7
Publikováno v:
Journal of the Geological Society of India. 82:207-216
Felsic tuff beds with some presumed sedimentary components were reported from the Owk Shale (Kurnool Group; bearing Neoproterozoic fossils) in the upper part of the sedimentary succession in the Cuddapah basin in India by Saha and Tripathy (2012a). O
Autor:
George D. Kamenov, Robert L. Bauer, Scott D. Samson, A.M. Satkoski, Paul A. Mueller, M. E. Bickford
Publikováno v:
Precambrian Research. 224:36-50
The 3.5–2.6 Ga rocks of the Minnesota River Valley (MRV) provide a unique opportunity to examine rocks that span the now recognized crucial time (3.2–3.0 Ga) on the Earth when Wilson style plate tectonic processes likely started. To elucidate the
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
The Journal of Geology. 120:477-485
A rhyolitic tuff with a minimum thickness of about 2.5 m occurs at the top of the sedimentary succession of the Indravati Group in south-central India. The tuff is a high-K, low-Na rhyolite with dominantly K-feldspar phenocrysts. Cathodoluminescence
Autor:
M. E. Bickford, Jack Hietpas, Ranjan Kumar Ray, Arunangshu Mukherjee, Juergen Schieber, Rajeeva Guhey, Purbasha Bhattacharya, Pratap Chandra Dhang, Abhijit Basu, Sarbani Patranabis-Deb
Publikováno v:
The Journal of Geology. 119:535-548
Magmatic zircons from two samples of the Dhamda Tuff in the Tarenga Formation of the Mesoproterozoic Chhattisgarh Supergroup in central India were dated by U-Pb SHRIMP methods, which yielded a concordia upper-intercept age of Ma. The samples are from
Publikováno v:
The Journal of Geology. 119:553-556
Publikováno v:
Geological Society of America Bulletin. 123:951-957
U/Pb detrital zircon ages from global modern river sediments define eight peak clusters centered at 2700, 2500, 2010, 1840, 1600, 1150, 600, and 300 Ma. These clusters extend vertically into both positive and negative e Hf (T) space and are similar t
Publikováno v:
The Journal of Geology. 119:33-50
The Indian Shield includes the Singhbhum, Bastar, and East and West Dharwar cratons. Proterozoic sedimentary basins formed on these cratons have preserved rocks with a range of degrees of metamorphism and deformation. In the Chhattisgarh Basin, withi
Publikováno v:
American Mineralogist. 95:1796-1806
Granulite-facies quartzites from the Adirondack Highlands (Grenville Province, New York) contain accessory zircon with ubiquitous metamorphic overgrowths. Detrital zircon cores are resorbed, preserve various internal zoning styles and inclusions, and