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Melrose Granite

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Journal Article
Journal: Geology
Published: 01 May 1989
Geology (1989) 17 (5): 391–394.
... lies within the compositionally homogeneous Melrose granite, which is undeformed to the west of the zone. The angle between C and S bands in mylonitic Melrose granite varies from 43° in the westernmost protomylonite to near 0° in the easternmost ultramylonite. Radon in the overlying soils increases...
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2399(05)
... in this area began when post-Acadian extension and granite intrusion initiated a period of half-graben development from New Brunswick to southern Newfoundland ( Marillier et al., 1989 ; Piper, 1994 ). The resulting depocenters are considered “basins” in their own right and together form the regional Maritimes...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 11 October 2017
Lithosphere (2017) 9 (6): 910–926.
... found in Upper Cambrian sandstones (from the Sauk II-III boundary) in the Wind River Canyon on the Wyoming craton, the Melrose area of the southwest Montana thrust belt, and the Leaton Gulch area of the central Idaho thrust belt. The detrital zircon signatures of these Upper Cambrian rocks is markedly...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.224.01.16
EISBN: 9781862394728
... zone from the southwestern Virginia Piedmont. Modified from Gates et al. (1986), Virginia Division of Mineral Resources (1993), and Henika (1997). Samples for this study were collected from a traverse along the Roanoke River. The Melrose granite is progressively transformed into mylonitic rocks...
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Journal Article
Journal: Economic Geology
Published: 01 December 2004
Economic Geology (2004) 99 (8): 1771–1780.
... to Rosalia Jenchuraeva for organizing the IGCP-373 field trip to the Kyrgyz Tien Shan ("Ore-bearing granites of Eurasia") in August 2001 when the ore samples for this study were collected. The Kumtor mine staff, especially Dwayne Melrose, is greatly acknowledged for access to the open pit and for assistance...
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Journal Article
Published: 01 August 1989
Journal of the Geological Society (1989) 146 (4): 575–596.
...Bernard Elgey Leake Abstract Although now largely disappeared within the 400 Ma-old Galway Granite, the syntectonic Connemara metagabbro–gneiss complex, which crystallized at 490 Ma (Arenig), is the largest intrusion into the Dalradian rocks. It is part of widespread Cambro–Ordovician volcanism...
Journal Article
Journal: Economic Geology
Published: 01 September 2013
Economic Geology (2013) 108 (6): 1397–1424.
.... Stratigraphic relationships, isotopic ages, hornblende barometry, and fluid inclusion data indicate that exposures of the Butte Granite, which hosts mineralization, crystallized at ~6- to 9-km depth and that early porphyry Cu-Mo deposits formed at similar depths of 5 to 9 km. A period of rapid uplift...
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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP464.13
EISBN: 9781786203724
... Bulgaria. Diverse lithologies are present, including granite, gneiss, quartzite, schist, shales and volcanic rock fragments. A Balkanides source supplied by the palaeo-Kamchia appears likely. The Samotino Melrose-1 location is with an offshore channel supplying sediment into the offshore basin. Photograph...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.246.01.02
EISBN: 9781862394940
... & Draper 1997 ; Hutton et al . 1998 ). Offshore plateaux adjacent to the Queensland coast are composed of granitic intrusions into Devonian metasediments similar to that of the North Queensland Orogen ( Feary et al . 1993 ). Between the Bancannia Trough and far north Queensland, the location...
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Journal Article
Published: 01 May 2013
Scottish Journal of Geology (2013) 49 (1): 33–40.
.... These Upper Palaeozoic rocks form relatively low-lying ground: to the north, the Lower Palaeozoic Ettrick Group outcrop continues to form the Lammermuir Hills; whilst to the south, the Cheviot massif is underpinned by Devonian andesitic lavas and a granite pluton ( Fig. 1 ). The effect of this geologically...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 August 2017
Economic Geology (2017) 112 (5): 1205–1230.
... as of June 30, 2016 ( Northern Star Resources Limited, 2016 ). Historically, Paulsens was known as the Melrose mine, which was active in the 1930s with reports of 916 ounces of gold recovered from 2,955 t of ore ( Forman, 1938 ; Blight, 1985 ; Northern Star Resources Limited, 2015b ). The geological...
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Journal Article
Published: 17 April 2019
Quarterly Journal of Engineering Geology and Hydrogeology (2019) 52 (3): 386–398.
... Mountain Road, while more limited classification testing was carried out on soil obtained from the Kaeo site, supplemented by data obtained by O'Sullivan (2009) for Ogles, Lentfer (2007) and Melrose & Willis (2010) for Silverdale, and the Further North Alliance (2013) for Puhoi. While...
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Journal Article
Published: 01 April 2005
Scottish Journal of Geology (2005) 41 (1): 3–11.
... mostly discharge at former Spa sites ( Robins & Ferry 1992 ). These include Bridge of Earn, south of Perth, which has a Cl concentration of 1250 mg 1 –1 , and the Na-dominated waters of Moffat, Innerleithen and Melrose in the Southern Uplands. Strathpeffer Spa, north of Inverness, is a young...
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Journal Article
Published: 17 February 2020
Scottish Journal of Geology (2020) 56 (1): 63–79.
... investigations of Rachel McRobert a hundred years ago. Near Melrose, the Eildon Hills ( Fig. 1 ) comprise a near-surface suite of sill-like bodies varying from augite olivine trachytes to alkali rhyolitic varieties ( McRobert 1914 ). These are also Tournaisian, dated ( 40 Ar/ 39 Ar) at 352 Ma ( Monaghan...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1973
AAPG Bulletin (1973) 57 (9): 1703–1713.
... and Clark Counties, southeastern Granite County, and in northern Deer Lodge and Jefferson Counties is in a tectonically complex area marginal to the plutonic province of the Boulder batholith and related stocks. Emmons and Calkins (1913 , p. 68) suggested that thinning was caused by nondeposition or pre...
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Journal Article
Published: 01 December 1979
Journal of the Geological Society (1979) 136 (6): 755–770.
... Fault GBF Gillespie Burn Fault GF Grassfield Fault HL Hawick Line HtL Hartfell Line KF Kingledores Fault LL Leadhills Line LRF Loch Ryan Fault MVFMoffat Valley Fault RL Riccarton Line SF Stinchar Fault SUF Southern Upland Fault TTZ Talnotry Thrust Zone Devonian granites: CCG Cairnsmore of Carsphairn CG...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.182.01.02
EISBN: 9781862394308
... of broad tracts of lowland. The geology of these lands is diverse and complex, with ages and lithologies ranging from Precambrian granite and metasediments, through Palaeozoic limestone, Permo-Triassic sandstone and Cretaceous Chalk, to Palaeogene volcanic rocks ( Fig. 1 ). Drift geology includes...
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Journal Article
Published: 01 August 1998
Journal of the Geological Society (1998) 155 (4): 627–637.
... Interaction (WRI-9) 1998 Rotterdam Balkema 215 218 Edmunds W.M. Andrews J.N. Burgess W.A. Kay R.L.F. Lee D.J. The evolution of saline and thermal groundwaters in the Carnmenellis granite Mineralogical Magazine 1984 48 407 424 Edmunds W.M. Cook J.M. Miles...
Journal Article
Published: 14 July 2016
Canadian Journal of Earth Sciences (2016) 53 (11): 1372–1415.
... Jurassic (190 Ma) sedimentary units, as well as Jurassic granite gneiss ( van Wyck and Williams 2002 ) ( Fig. 2C ). The lower plate also contained, in the Papuan Peninsula to the east, a 3–4 km sequence of MORB-like submarine basalts, gabbros, and sedimentary rocks, referred to in places as the Milne...
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Journal Article
Published: 01 May 2013
Scottish Journal of Geology (2013) 49 (1): 59–77.
... granite (Drygalski Fjord Complex and minor associated metasedimentary formations), Upper Jurassic lavas and volcaniclastic rocks (Larsen Harbour Complex), and Lower Cretaceous tuff (Annenkov Island Formation). In total, the geology of South Georgia illustrates an active continental margin split...
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