Zobrazeno 1 - 10
of 66
pro vyhledávání: '"Victor A. Gostin"'
Autor:
A.P. Belperio, Victor A. Gostin, Colin V. Murray-Wallace, J. H. Cann, William A Nicholas, Anthony Dosseto, Yusuke Yokoyama, Tsun You Pan, Terry J. Lachlan
Publikováno v:
Quaternary Science Reviews. 259:106899
In contrast to the detection and resolution of Late Pleistocene interstadials (Marine Isotope Stages; MIS 5c, 5a and 3) in marine and ice core-based oxygen isotope records, accurately defining palaeosea-levels for these events from sea level indicato
Publikováno v:
Australian Journal of Earth Sciences. 60:463-474
Alluvial-channel and overlying eolian deposits exposed in coastal cliffs in the Port Campbell australite (Australian tektite) strewn field, SW Victoria, were studied stratigraphically and dated by optically stimulated luminescence (OSL) for quartz sa
Publikováno v:
Episodes. 35:226-235
The Flinders Ranges and its surroundings in South Australia comprise an impressive rugged terrain that rises abruptly from piedmont plains to the east and west and merges into the plains of the Cenozoic Lake Eyre Basin to the north. Folded and faulte
Autor:
Katherine A. Bron, Victor A. Gostin
Publikováno v:
Meteoritics & Planetary Science. 47:296-318
–Ejecta from the large subsurface Tookoonooka impact structure have been foundin the Lower Cretaceous strata of the extensive Eromanga Basin of centralAustralia. Observations from 31 wells spanning 400,000 km 2 of the basin provide compellingeviden
Publikováno v:
Geological Society, London, Memoirs. 36:673-676
Sedimentary features characteristic of ice-rafting are present in the Bunyeroo Formation (Wilpena Group) of the Adelaide Geosyncline and in the coeval Dey Dey Mudstone (Ungoolya Group) of the eastern Officer Basin (Figs 66.1 & 66.2), providing eviden
Autor:
Victor A. Gostin, George E. Williams, Phillip W. Schmidt, David M. McKirdy, Wolfgang V. Preiss
Publikováno v:
Geological Society, London, Memoirs. 36:713-721
Deposits of the late Cryogenian Elatina glaciation constitute the Yerelina Subgroup in the Adelaide Geosyncline region, South Australia. They have a maximum thickness of c . 1500 m, cover 200 000 km 2 , and include the following facies: basal boulder
Autor:
George E. Williams, Wolfgang V. Preiss, Paul M. Ashley, Victor A. Gostin, Philip W. Schmidt, David M. McKirdy
Publikováno v:
Geological Society, London, Memoirs. 36:701-712
The record of two Neoproterozoic glaciations in South Australia has been known for about a century. The earlier glaciation, of Sturtian age, is represented by the Yudnamutana Subgroup and is characterized by widespread diamictites with both intrabasi
Publikováno v:
Australian Journal of Earth Sciences. 57:859-869
Isolated quartzose pebbles, clusters of quartz granules, orthogonal aggregates of poorly sorted quartzose coarse sand, and ovoid pellets (≤2 mm long) of quartz silt occur in hemipelagic marine mudstone of the mid-Ediacaran Bunyeroo Formation expose
Autor:
Edward J. Rhodes, Frances M. Williams, Martin Williams, David Haberlah, Geraldine Jacobsen, Steven M. Hill, Peter Glasby, Anthony O'Flaherty, Victor A. Gostin
Publikováno v:
Geological Society, London, Special Publications. 346:185-223
David Haberlah, Peter Glasby, Martin A. J. Williams, Steven M. Hill, Frances Williams, Edward J. Rhodes, Victor Gostin, Anthony O'Flaherty and Geraldine E. Jacobsen
Publikováno v:
Precambrian Research. 163:307-331
The late Cryogenian Elatina glaciation in South Australia, of Marinoan age, is named after the Elatina Formation of the glaciogenic Yerelina Subgroup, which covers ∼200,000 km2 in the Adelaide Geosyncline and on the cratonic Stuart Shelf and is up