Zobrazeno 1 - 10
of 66
pro vyhledávání: '"Robert T. Gregory"'
Publikováno v:
American Journal of Science. 322:533-560
Ophiolite complexes represent fragments of ocean crust and mantle formed at spreading centers and emplaced on land. The setting of their origin, whether at mid-ocean ridges, back-arc basins, or forearc basins has been debated. Geochemical classificat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2763edba89265fea43c9fec8339aa8c8
https://doi.org/10.1130/2021.2552(01)
https://doi.org/10.1130/2021.2552(01)
Autor:
Robert T. Gregory
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Robert T. Gregory
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Barun K. Mukherjee, Koushick Sen, Satadru Bhattacharya, Souvik Das, Robert T. Gregory, Franco Marcantonio, Asish R. Basu
Publikováno v:
Chemical Geology. 551:119772
Ophicarbonates are found in ophiolite-associated peridotites and bear signature of fluid-rock interaction either on ocean floor or during ophiolite emplacement. The occurrence of ophicarbonate veins hosted by ultramafic rocks of the Indus Ophiolite,
Autor:
Robert T. Gregory
Publikováno v:
International Geology Review. 61:1294-1295
Graham Park is an Emeritus Professor from the University of Keele, United Kingdom, who has published textbooks for geology professionals on subjects such as the Foundations of Structural Geology (1...
Autor:
Robert T. Gregory, Robert G. Coleman
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Analytical Biochemistry. 372:213-221
A method to determine 18 O kinetic isotope effects (KIEs) in the hydrolysis of GTP that is generally applicable to reactions involving other nucleotide triphosphates is described. Internal competition, where the substrate of the reaction is a mixture
Publikováno v:
The Journal of Geology. 113:611-626
Igneous zircons in felsic schist, or metatuff, infolded with mafic schist, calcschist, and quartz mica schist of the As Sifah lower plate window, NE Oman, have yielded a U/Pb SHRIMP crystallization age of \documentclass{aastex} \usepackage{amsbsy} \u
Publikováno v:
Journal of Structural Geology. 27:371-374