Ax-les-Thermes Granite

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Journal Article
Published: 01 April 1993
European Journal of Mineralogy (1993) 5 (2): 341–351.
Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.5
EISBN: 9781862396814
... for some ages, especially for ages as old as 337 Ma for a few granite bodies (i.e. Ax-les-Thermes and Bossòst). The last deformation event (D 3 ) corresponds to localization of the deformation during cooling of the Variscan crust, leading to east–west- to NW–SE-trending mylonitic bands with reverse...
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Journal Article
Published: 01 January 1964
Bulletin de la Société Géologique de France (1964) S7-VI (1): 69–86.
...E. Raguin Abstract The Aston gneiss-migmatite massif (Hercynian) on the headwaters of the Ariege river in southern France is made up of the Riete augen gneiss, small bodies of the Peyregrand gneiss to the south and southwest, and migmatite bordering these except on the north. The Ax-les-Thermes...
Journal Article
Published: 01 May 2009
Bulletin de la Société Géologique de France (2009) 180 (3): 199–207.
... along the Ariège valley and east of Ax-les-Thermes. The Hospitalet dome has a core of relatively homogeneous biotite orthogneiss of monzogranitic origin with dimensions of 28 km by 9 km wide [ van den Eeckhout, 1986 ]. Smaller bodies of peraluminous granite and lenses of calc-alkaline granites...
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Journal Article
Published: 29 November 2017
Bulletin de la Société Géologique de France (2017) 188 (6): 36.
... Thermes ( Fig. 1 ), but the authors acknowledge that only segments of this complex P-T evolution can be documented, the second prograde path remaining conjectural. Le Rhodope est un complexe métamorphique de haut grade situé à la frange Nord de la région égéenne. De nombreux scénarios ont été...
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Journal Article
Journal: Economic Geology
Published: 01 March 2018
Economic Geology (2018) 113 (2): 309–345.
... amphibolite, interspersed bodies of megacrystic plagioclase-microcline orthogneiss, and fine-grained to aplitic granite gneiss ( Kockel et al., 1977 ; Kalogeropoulos et al., 1989 ; Nebel et al., 1991 ; Gilg and Frei, 1994 ). These lithologic units have an arcuate geometry, striking in a north-south...
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Journal Article
Published: 01 September 2010
Bulletin de la Société Géologique de France (2010) 181 (5): 411–428.
...-320 Ma, viennent d’être proposés pour des intrusions qui seraient synchrones de MII. C’est le cas du granite peralumineux syn-D2a d’Ax-les-Thermes, au flanc nord du dôme de l’Aston (321 ± 7 Ma ; Denèle [2007] ) et d’un sill dioritique du massif des Guilleries (323,6 ± 2,8 Ma ; Martínez et al...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2002
DOI: 10.1144/GOSPP.8
EISBN: 9781862393912
... several types of mafic or accessory minerals. Textures can also be very variable ranging from aplitic to coarse grained (pegmatitic). The largest plutons are usually medium grained and have a homogeneous texture (e.g. Ax-les-Thermes granite). Muscovite or two-mica leucogranites are the most widespread...
Series: Geological Society, London, Special Publications
Published: 01 January 2003
DOI: 10.1144/GSL.SP.2003.210.01.04
EISBN: 9781862394582
... and 35 Ma ( Mercier et al. 1987 ; Le Pichon et al. 1992 ) India has continued its northward motion at reduced velocity and acts as a rigid indenter penetrating (for ∼2000 km) into Asia to cause post-collisional underplating (India) and uplift (Tibet) ( Molnar and Tapponnier 1978 ; Cobbold and Davy...
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Journal Article
Published: 01 December 1993
Bulletin of the Seismological Society of America (1993) 83 (6B): 2059–2240.
... in Northern Baja California ReboCJ -75 1371 nts and crustal Q on LE ATTENUATION in Southern Mexico using the CanaJA -78 1807 / The apparent s and short-period wave ATTENUATION in the Canadian Shield ChunKY -79 1039 ent in Central Italy / ATTENUATION in the crust beneath central CampM -15 1395 region...
Series: Geophysical References Series
Published: 01 January 2002
DOI: 10.1190/1.9781560801979.ch1
EISBN: 9781560802969
... Figures A-18 , A-19 , and E-10 . At least one of the electrodes is usually at the surface. Abelian : ( ∂ bē' ∂ n or ∂ bēl' y ∂ n) Commutative (q.v.). Named for Niels Henrik Abel (1802–1829), Norwegian mathematician. abnormal end : Premature termination of a computer program caused...
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