Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Marshall C. Palmer"'
Autor:
James M. Scott, Marianne Negrini, Kevin Faure, Marshall C. Palmer, Derek R. Knaack, Matthew I. Leybourne
Publikováno v:
Meteoritics & Planetary Science. 58:328-340
Autor:
Marshall C. Palmer, James M. Scott, Steven A.F. Smith, Petrus J. le Roux, Chris Harris, Marianne Negrini, Matthew S. Tarling
Publikováno v:
Earth and Planetary Science Letters. 614:118188
Autor:
Sarah Woodland, James M. Scott, D. Graham Pearson, Jingao Liu, Malcolm R. Reid, Alan Cooper, Marshall C. Palmer, Dongxu Li, Andreas Auer, Stephen E. Read
Publikováno v:
Geochimica et Cosmochimica Acta. 312:25-43
Osmium isotopes, whole rock and mineral geochemical data from peridotite xenoliths from two Miocene McMurdo Volcanic Group cinder cones in the Transantarctic Mountains (TAM) in Southern Victoria Land, Antarctica, reveal that the underlying mantle pre
Publikováno v:
New Zealand Journal of Geology and Geophysics. 64:89-106
The occurrence, concentration and geochemistry of REE-bearing minerals in beach sands along the West Coast of the South Island of New Zealand is reported as a proxy for the composition of adjacent ...
Autor:
Marshall C. Palmer, Emma J. Scanlan, James M. Scott, Lauren Farmer, Daniel Pickering, Victoria J. Wilson, Marcus Oelze, Dave Craw, Petrus J. le Roux, Yan Luo, D. Graham Pearson, Malcolm R. Reid, Claudine H. Stirling
Publikováno v:
Ore Geology Reviews
The Otago Schist in New Zealand hosts orogenic tungsten (W) mineralization in two types. Proximally-sourced (“proximal”) mineralization in sub- to lower-greenschist facies Mesozoic metasedimentary rocks within the northern flank of the Otago Schi
Publikováno v:
Journal of Geochemical Exploration. 224:106760
Scheelite (CaWO4) is a useful mineral in determining the paragenesis of mineralising systems. While it is well-established that scheelite grains contain trace element budgets indicative of the mineralising fluid, scheelite grains within the same rock
Publikováno v:
New Zealand Journal of Geology and Geophysics. 58:22-32
The peak conditions and timing of metamorphism have been determined for the early Paleozoic Greenland Group in south Westland, New Zealand. The Greenland Group, which is the most extensive pre-Cenozoic unit west of the Alpine Fault in Westland, is do