Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Paul F. Carr"'
Publikováno v:
Rocks & Minerals. 95:210-233
Tsumeb is one of the world’s premier localities for arsenate (and arsenite) minerals. At least eighty-four species containing the arsenate (or arsenite) anion groups have been confirmed from Tsumeb...
Autor:
Dat T. Pham, Chris Gouramanis, Adam D. Switzer, Charles M. Rubin, Brian G. Jones, Kruawun Jankaew, Paul F. Carr
Publikováno v:
Marine Geology. 396:79-99
Publikováno v:
Gondwana Research. 51:149-169
The isotopic, geochemical, and physical characteristics of the Late Permian mass extinction have been identified and assessed from terrestrial sections across the Sydney Basin, eastern Australia. These new data are used to both correlate the extincti
Autor:
Brian G. Jones, D. T. Pham, Paul F. Carr, Kruawun Jankaew, Adam D. Switzer, Chris Gouramanis, Charles M. Rubin
Publikováno v:
Marine Geology. 385:274-292
Sediment records left by coastal hazards (e.g. tsunami and/or storms) may shed light on the sedimentary and hydrodynamic processes happening during such events. Modern onshore and offshore sediment samples were compared with the 2004 Indian Ocean Tsu
Publikováno v:
Chemical Geology. :174-188
The identification of the Permian–Triassic boundary (PTB) and Permian–Triassic mass extinction event (PTME) in eastern Australia is based primarily on palynological and plant fossil evidence with limited δ 13 C org data from the northern part of
Publikováno v:
Lithos. 151:46-56
The Mt Gibraltar intrusion near Mittagong and Bowral in New South Wales, Australia (lat. 34°27′54″S, long. 150°25′44″) is a small intrusive body of hypersolvus microsyenite emplaced into the Triassic Hawkesbury Sandstone of the Sydney Basin
Publikováno v:
Quaternary Geochronology. 5:1-9
Cosmogenic 21 Ne was utilised to determine exposure ages of young subaerial basaltic lava flows from the Newer Volcanic Province, western Victoria, Australia. The ages (36–53 ka) determined from co-existing cosmogenic 21 Ne and 3 He in olivines sep
Publikováno v:
Journal of Asian Earth Sciences. 37:31-41
Small lensoidal bodies of massive and disseminated chromitites have been examined in association with ultramafic rocks of the Mawat ophiolite complex (MOC), Iraqi Zagros Thrust Zone, northeastern Iraq. The chromitites are surrounded by dunite envelop
Publikováno v:
The Canadian Mineralogist. 46:73-85
Native lead, a rare mineral, occurs in a late-stage vein in the world’s largest lead – zinc – silver deposit, at Broken Hill, Australia. The lead-bearing vein consists mainly of laumontite, quartz, biotite and muscovite, together with minor amo
Publikováno v:
Journal of Sedimentary Research. 77:980-991
Calcite pseudomorphs after ikaite (glendonite) are associated with coldwater depositional systems, including glaciomarine and deepwater settings, as dictated by the limited stability field of ikaite. Ikaite precipitation is favored by elevated alkali