Zobrazeno 1 - 10
of 171
pro vyhledávání: '"Richard Glen"'
Publikováno v:
Geological Society, London, Special Publications. 533:545-557
Evidence of Early Ordovician deposition and intrusion in East Antarctica is best known from the Ross Orogen, postdating the 495–489 Ma Ross Orogeny. Here, c. 490–475 Ma granites (with related dykes and sills) of the Granite Harbour Intrusives rep
Publikováno v:
Australian Journal of Earth Sciences. 69:406-418
Akademický článek
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Autor:
Ryan Kilburn, Eric T. Fedosejevs, Devang Mehta, Mina Ghahremani, Jay J. Thelen, Richard Glen Uhrig, Wayne A. Snedden, William Charles Plaxton
Publikováno v:
SSRN Electronic Journal.
Autor:
Boire, Richard Glen
Publikováno v:
The Independent Review, 2002 Oct 01. 7(2), 253-258.
Externí odkaz:
https://www.jstor.org/stable/24562670
Autor:
Timothy Chapman, J. Kalmbach, P. M. Ashley, L. A. Milan, Richard Glen, Elena Belousova, B. Fu
Publikováno v:
Geophysical Research Letters. 48
Publikováno v:
Goldschmidt Abstracts.
Autor:
Richard Glen, Roger A. Cooper
Publikováno v:
Earth-Science Reviews. 220:103687
New insights into the Late Precambrian-latest Devonian evolution of the Pacific margin of Gondwana are obtained by treating the margin in terms of three key tectonic elements: i) the in situ part of the Ross Orogen of Eastern Antarctica (Wilson Terra
Publikováno v:
Australian Journal of Earth Sciences. 64:143-224
Lower to upper Middle Ordovician quartz-rich turbidites form the bedrock of the Lachlan Orogen in the southern Tasmanides of eastern Australia and occupy a present-day deformed volume of ∼2–3 million km3. We have used U–Pb and Hf-isotope analys
Publikováno v:
Canadian Journal of Earth Sciences. 53:1372-1415
Non-collisional, convergent margin orogens are generally called accretionary orogens, although there may not have been horizontal accretion across the plate boundary. We revive the term non-collisional orogen and use a Gondwanaland perspective to dis