Works matching IS 17556910 AND DT 2009 AND VI 100 AND IP 1/2
Results: 19
TRE volume 100 issue 1-2 Cover and Front matter.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. f1, doi. 10.1017/S1755691009999996
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- Article
TRE volume 100 issue 1-2 Cover and Back matter.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. b1, doi. 10.1017/S1755691009999984
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- Article
Preface.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. v, doi. 10.1017/S175569100901620X
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Plutonism versus Neptunism at the southern tip of Africa: the debate on the origin of granites at the Cape, 1776–1844.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 1, doi. 10.1017/S1755691009016193
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Similarities between mantle-derived A-type granites and voluminous rhyolites in continental flood basalt provinces.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 51, doi. 10.1017/S1755691009016181
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Crustal melt granites and migmatites along the Himalaya: melt source, segregation, transport and granite emplacement mechanisms.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 219, doi. 10.1017/S175569100901617X
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Four-stage building of the Cambrian Carion pluton (Madagascar).
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 133, doi. 10.1017/S1755691009016156
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The evolution of late-Hercynian granites and rhyolites documented by quartz – a review.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 185, doi. 10.1017/S1755691009016144
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The geochemistry of Archaean plagioclase-rich granites as a marker of source enrichment and depth of melting.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 35, doi. 10.1017/S1755691009016132
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The sanukitoid series: magmatism at the Archaean–Proterozoic transition.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 15, doi. 10.1017/S1755691009016120
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Structural controls on melt segregation and migration related to the formation of the diapiric Schwerin Fold in the contact aureole of the Bushveld Complex, South Africa.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 61, doi. 10.1017/S1755691009016119
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Trace element constraints on mid-crustal partial melting processes – A garnet ionprobe study from polyphase migmatites (Damara orogen, Namibia).
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 205, doi. 10.1017/S1755691009016107
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Zoning and resorption of plagioclase in a layered gabbro, as a petrographic indicator of magmatic differentiation.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 235, doi. 10.1017/S1755691009016090
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Emplacement and assembly of shallow intrusions from multiple magma pulses, Henry Mountains, Utah.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 117, doi. 10.1017/S1755691009016089
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Causes of compositional diversity in a lobe of the Half Dome granodiorite, Tuolumne Batholith, Central Sierra Nevada, California.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 173, doi. 10.1017/S1755691009016065
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Chemical structure in granitic magmas – a signal from the source?
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 159, doi. 10.1017/S1755691009016053
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Granite formation: Stepwise accumulation of melt or connected networks?
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 105, doi. 10.1017/S175569100901603X
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Anisotropy of magnetic susceptibility fabrics in syntectonic plutons as tectonic strain markers: the example of the Canso pluton, Meguma Terrane, Nova Scotia.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 147, doi. 10.1017/S1755691009016028
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Parental magmas of Grenville Province massif-type anorthosites, and conjectures about why massif anorthosites are restricted to the Proterozoic.
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- Earth & Environmental Science Transactions of the Royal Society of Edinburgh, 2009, v. 100, n. 1/2, p. 77, doi. 10.1017/S1755691009016016
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