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CROWLEY, QUENTIN G (6)
Cooper, M.R. (1)Henney, P.J. (1)Hollis, S.P. (1)Noble, S.R. (1)SubjectGeology (3)Batholith (1)East Java (1)Grampian (1)Late Caledonian (1)lattice distortion (1)Magmatism (1)Ophiolites (1)Pennine (1)Slab break-off (1)... View MoreDate Issued2013 (4)2010 (1)2011 (1)Has File(s)Yes (6)

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A Toba-scale eruption in the Early Miocene: the Semilir eruption, East Java, Indonesia 

CROWLEY, QUENTIN G (2011)
The Indonesian archipelago is well known for volcanic activity and has been the location of three catastrophic eruptions in the last million years: Krakatau, Tambora and Toba. However, there are no reports of large magnitude ...
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New U-Pb age constraints for the Laxford Shear Zone, NW Scotland: Evidence for tectono-magmatic processes associated with the formation of a Paleoproterozoic supercontinent 

CROWLEY, QUENTIN G (2013)
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A U-Pb age for the Late Caledonian Sperrin Mountains minor intrusions suite in the north of Ireland: timing of slab break-off in the Grampian terrane and the significance of deep-seated, crustal lineaments 

CROWLEY, QUENTIN G; Cooper, M.R.; Hollis, S.P.; Noble, S.R.; Henney, P.J. (2013)
An intrusion of trachy-andesite, representative of a newly discovered suite of high-K–Ba–Sr, calc-alkaline minor intrusions (termed herein the Sperrin Mountains suite), hosted within the Grampian terrane in the north of ...
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The North Pennine batholith (Weardale Granite) of northern England new data on its age and form 

CROWLEY, QUENTIN G (2010)
A three-dimensional gravity model of the North Pennine batholith is interpreted to indicate that it comprises five contiguous steep-sided plutons. The North Pennine batholith was previously referred to as the Weardale ...
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Lattice distortion in a zircon population and its effects on trace element mobility and U-Th-Pb isotope systematics: examples from the Lewisian Gneiss Complex, northwest Scotland 

CROWLEY, QUENTIN G (2013)
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U-Pb zircon ages for Yarlung Tsangpo suture zone ophiolites, southwestern Tibet and their tectonic implications 

CROWLEY, QUENTIN G (2013-09-03)

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