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Barrington Tops Granodiorite

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Journal Article
Published: 01 December 1986
American Mineralogist (1986) 71 (11-12): 1314-1321.
...Douglas R. Mason Abstract Small inclusions of hypersthene, augite, hornblende, and Fe-Ti oxides occur in plagioclase cores of granitoids from the Permian Barrington Tops Granodiorite, New South Wales. Mineralogically and chemically the ferromagnesian inclusions match larger discrete grains...
Journal Article
Published: 01 May 1991
Canadian Journal of Earth Sciences (1991) 28 (5): 743-753.
..., and pyroxenite, which together with tonalite make up the DIS. Some of the petrological characteristics of the suite are unusual, but known from other regions: ( i ) some felsic magmatic rocks in the southern Sierra Nevada and Barrington Tops (Australia) batholiths contain primary orthopyroxene; ( ii ) goblet...
Journal Article
Published: 01 June 2014
South African Journal of Geology (2014) 117 (1): 149-171.
...S. JUNG; J. BERNDT; A. STRACKE; F. HAUFF; N. KASTEK Abstract The Tsomtsaub pluton (central Damara orogen, Namibia) consists of quartz diorites, granodiorites and granites. Intrusion ages of the undeformed and unmetamorphosed quartz diorites and granites are constrained by LA-ICP-MS U-Pb zircon...
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Journal Article
Published: 01 September 2010
Journal of the Geological Society (2010) 167 (5): 915-941.
...J.D. Clemens; K. Benn Abstract: The Late Devonian, high-level, post-orogenic Mt Disappointment pluton was emplaced as a nested laccolith. Field observations and magnetic fabric (anisotropy of magnetic susceptibility) data show that the monzogranitic to granodioritic magmas entered the pluton from...
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Image
Schematic time-space diagram for the New England segment of the Terra Austr...
Published: 01 November 2011
., 2007 ); 13—Greymare Granodiorite ( Donchak et al., 2007 ); 14—Barrington Tops Granodiorite ( Table 1 ); 15—Duncans Creek Trondhjemite ( Table 1 ); 16—Nambucca slate belt argon mica ages ( Offler and Foster, 2008 ). Contractional and extensional events in basins west of New England are from Korsch et
Image
Geological map of the southern New England region of the Terra Australis or...
Published: 01 November 2011
; BT—Barrington Tops Granite; C—Connors arc; CM—Clarence Moreton Basin; D—D'Aguilar block; DG—Dundurrabin Granodiorite; DT—Duncans Creek Trondhjemite; ECB—Emu Creek block; G—Glenmore; GB—Gresford block; GB (inset)—Gunnedah Basin; GG—Greymare Granodiorite; GL—Glenburnie Leuco-adamellite; H—Hastings
Journal Article
Journal: GSA Bulletin
Published: 01 November 2011
GSA Bulletin (2011) 123 (11-12): 2240-2255.
...., 2007 ); 13—Greymare Granodiorite ( Donchak et al., 2007 ); 14—Barrington Tops Granodiorite ( Table 1 ); 15—Duncans Creek Trondhjemite ( Table 1 ); 16—Nambucca slate belt argon mica ages ( Offler and Foster, 2008 ). Contractional and extensional events in basins west of New England are from Korsch et...
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Journal Article
Journal: Geosphere
Published: 01 April 2010
Geosphere (2010) 6 (2): 130-159.
... Devil Lake pluton ( Tobisch et al., 1995 ), the Turner Lake pluton, and the ca. 88 Ma megacrystic facies of the Half Dome granodiorite, which is part of the Tuolumne batholith ( Fleck and Kistler, 1994 ; Gray, 2003 ). The JLP intrudes the 99 ± 1 Ma Illilouette Creek pluton to the west ( Tobisch et al...
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Journal Article
Published: 01 April 2000
The Canadian Mineralogist (2000) 38 (2): 345-378.
.... 1994 ). In the east (Utsalik domain), Nd isotopic signatures of granodiorites indicate significant involvement of older crust, whereas in the west (Lake Minto domain), rocks of similar age and composition are relatively juvenile isotopically. The western Minto block was reworked during a second...
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Journal Article
Journal: Economic Geology
Published: 01 June 2014
Economic Geology (2014) 109 (4): 827-858.
... ; McMillan et al., 2009 ). It is elliptical and elongated slightly west of north and comprises four nearly concentric main intrusive phases ranging in composition from diorite to granodiorite ( McMillan, 1976 ; Casselman et al., 1995 ) and younging from the margin (211.3 ± 0.7 Ma) to core (209.2 ± 0.7 Ma; W...
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