Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Caroline Jane Forbes"'
Publikováno v:
Journal of Geochemical Exploration. 156:10-33
Light rare earth elements (LREEs) are commonly enriched within iron oxide-copper-gold (IOCG) deposits within the Gawler Craton, South Australia. The LREEs are host within a number of phases including monazite, which is a resistate phase that can with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2fdee15d1525bfe4bb5db6109bb5e791
https://doi.org/10.1016/j.gexplo.2015.04.011
https://doi.org/10.1016/j.gexplo.2015.04.011
Autor:
N Chalmers, Rian Dutch, David Giles, Caroline Jane Forbes, Peter G Betts, Martin Hand, Kazuhiro Suzuki
Publikováno v:
Precambrian Research. 185:65-85
We present metamorphic analysis from a porphyroblastic garnet–cordierite–spinel pelite from the Palaeo-Mesoproterozoic Mount Woods Inlier in South Australia. Petrographic analysis combined with a series of P – T pseudosections representative of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8be00912004424fee93498cbb9395308
https://doi.org/10.1016/j.precamres.2010.12.002
https://doi.org/10.1016/j.precamres.2010.12.002
Publikováno v:
Monash University
In situ SHRIMP U‐Pb analysis of monazite grains from pelites within an early‐formed high‐temperature shear zone in the southern Broken Hill Block, Australia, has been used to constrain the timing of prograde amphibolite facies and peak granulit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8a25a05fd58c5819a3aa2000496fdd4e
https://doi.org/10.1086/521611
https://doi.org/10.1086/521611
Publikováno v:
Journal of Metamorphic Geology. 23:745-770
The prograde pressure–temperature (P–T) path for the complexly polydeformed Proterozoic Broken Hill Block (Australia) has been reconstructed through detailed structural analysis in conjunction with calculation of compositionally specific P–T ps
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::399dd02a992d5eee224da17383699e16
https://doi.org/10.1111/j.1525-1314.2005.00608.x
https://doi.org/10.1111/j.1525-1314.2005.00608.x
Autor:
Caroline Jane Forbes, Peter G Betts
Publikováno v:
Australian Journal of Earth Sciences. 51:173-188
A north‐south‐trending relatively high‐strain shear zone active during the earliest stages of the ca 1.60–1.58 Ga Olarian Orogeny bounds domains characterised by different structural geometries in the northern Broken Hill Block. To the west o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::804c059b12ecfc91dab8cf9816f5ce41
https://doi.org/10.1111/j.1440-0952.2004.01051.x
https://doi.org/10.1111/j.1440-0952.2004.01051.x
Publikováno v:
Journal of Structural Geology. 26:113-126
Synchronous development of Type 2 and Type 3 fold interference patterns occur in the poly-deformed Broken Hill Inlier. The interference patterns have resulted from the superposition of recumbent F2 folds and ∼N–S-oriented upright F3 folds. The sy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1da38259d2ab93c29aeda92221fa343
https://doi.org/10.1016/s0191-8141(03)00074-9
https://doi.org/10.1016/s0191-8141(03)00074-9
The Ongole Domain in the southern Eastern Ghats Belt of India formed during the final stages of Columbia amalgamation at ca. 1600 Ma. Yet very little is known about the protolith ages, tectonic evolution or geographic affinity of the region. We prese
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b19b175070dd6cfd2088e5756eda5d8b
https://hdl.handle.net/11541.2/115292
https://hdl.handle.net/11541.2/115292
Autor:
John Foden, Helen Anne Williams, Bruce F. Schaefer, David Giles, Neil Colin Chalmers, Peter G Betts, Geordie Mark, Quinton Geoffrey Hills, Caroline Jane Forbes, M. J. Pankhurst
Publikováno v:
Tectonics. 28
[1] Tectonic models for the latest Paleoproterozoic to earliest Mesoproterozoic evolution of eastern Australia (circa 1620–1500 Ma) are diverse and either emphasize plume or plate margin activity, neither of which satisfactorily explains all geolog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba5ba4cc85e679201d0a3e267019c015
https://doi.org/10.1029/2008tc002325
https://doi.org/10.1029/2008tc002325
The origin of high temperatures during regional low-pressure granulite facies metamorphism within the Proterozoic Broken Hill Block, Australia, has been reinterpreted to be the result of burial of anomalously hot rock packages for which the lithosphe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dc1cbfabff63c2f37e4ccf5a8d0dd228
https://hdl.handle.net/11541.2/122033
https://hdl.handle.net/11541.2/122033
Autor:
Anthony J. Crawford, Irina Borissova, Nicholas G. Direen, Millard F. Coffin, Caroline Jane Forbes, Jacqueline A. Halpin
Publikováno v:
Geology. 36:807
The origin of the submarine Naturaliste Plateau off the southwestern coast of Australia is controversial; previous work supports both oceanic and continental affinities for the basement to volcanic and sedimentary sequences. We report the first evide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3c1ff4204df58f2c9482a5b1563b4085
https://doi.org/10.1130/g25059a.1
https://doi.org/10.1130/g25059a.1