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Capdevila Formation

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Journal Article
Published: 01 May 1999
Journal of Paleontology (1999) 73 (3): 394–402.
...D. Garcia-Bellido Capdevila; S. Conway Morris Abstract Two new fossil worms are described from the Lower Cambrian Kinzers Formation of southeast Pennsylvania. Both are unique specimens. Kinzeria crinita new genus and species has a body divided into three regions. The head bears a prominent set...
Journal Article
Published: 01 May 2004
Journal of Paleontology (2004) 78 (3): 431–455.
... Formation is 220 m thick, but it is from the lower 30 m that the fossil sponges were collected. These lower beds are primarily marls and shales, with some intercalated decimeter-thick limestone beds. Sánchez de Posada et al. (1998) and García-Bellido Capdevila (1999) described an abundant fossil...
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Journal Article
Published: 30 April 2018
Bulletin de la Société Géologique de France (2018) 189 (2): 7.
...Jacques Kornprobst; Benito Àbalos; Pierre Barbey; Anne-Marie Boullier; Jean-Pierre Burg; Ramon Capdevila; Stefan Claesson; Umberto Cordani; David Corrigan; Roy H. Gabrielsen; José I. Gil-Ibarguchi; Åke Johansson; Dominik Letsch; Philippe Le Vigouroux; Brian Upton This work is a review of Boris...
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Journal Article
Published: 01 January 1962
Bulletin de la Société Géologique de France (1962) S7-IV (1): 13–17.
...Raymond Capdevila Abstract The middle Pleistocene volcanic complex between Bessan and Saint Thibery (France) is composed of basanite volcanic material. Three main formations are recognized: tuffs, cones, and flows. Petrographic analysis of the material shows that the basanite is slightly deficient...
Image
Figure  11 — Ascospongiella <b>capdevilae</b>  n. gen. and sp., Villafeliz, León;...
Published: 01 May 2004
Figure 11 — Ascospongiella capdevilae n. gen. and sp., Villafeliz, León; San Emiliano Formation, late Bashkirian, Upper Carboniferous. 1, 99VI– 7A, holotype, longitudinal section of the specimen, showing the wide open spongocoel and the thickness of the body wall; light-colored, arched
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2001.200.01.06
EISBN: 9781862396081
... Gresens (1967) and Grant (1986) methods on phengite selvage/host-rock pairs, in order to estimate mass transfers involved in vein formation. Chemical analyses are given in Table 1 . For each sample pair, we compared the results of this approach with those of staining experiments and of mineral...
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Journal Article
Published: 15 August 2014
Geological Magazine (2015) 152 (2): 341–350.
... U–Pb SHRIMP-RG zircon dating The Ollo de Sapo Formation (Parga-Pondal, Matte & Capdevila, 1964 ) is the largest accumulation of pre-Variscan igneous rocks in the Iberian Peninsula. It crops out at the core of an antiform, the Ollo the Sapo anticlinorium, which extends...
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Journal Article
Published: 01 September 1992
Journal of the Geological Society (1992) 149 (5): 829–840.
... Tectonics 1983 2 345 556 Bullard E. Everett J. E. Smith A. G. The fit of continents around the Atlantic Royal Society of London Philosophical Transactions 1965 258 41 51 Capdevila R. Mougenot D. The pre-mesozoic basement of the western Iberian continental margin...
Journal Article
Published: 01 March 2001
Journal of Sedimentary Research (2001) 71 (2): 318–333.
...Luis M. Castañares; Sergio Robles; Domingo Gimeno; Jose C. Vicente Bravo Abstract The Errigoiti Formation, located in the central domain of the Basque-Cantabrian basin, is an Albian to Santonian bathyal submarine volcanic system of alkali basaltic character. These volcanics occurred...
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Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.5
EISBN: 9781862396814
... The Variscan segment of the Pyrenees is an interesting case study for tackling this question because crustal flow and dome formation are grossly coeval with emplacement of granite plutons and the structural features of both the middle and upper crustal levels are rather well documented...
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Journal Article
Published: 01 October 2009
Bulletin de la Société Géologique de France (2009) 180 (6): 529–544.
... that recorded the denudation of an early relief have generally been removed by erosion. In the Chalonnes area (southeast of the Armorican Massif), the reefal carbonates of the Chalonnes Formation (Fm) are overlain by the immature, poorly-sorted sandstones of the Sainte-Anne Fm. This formation is characterised...
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Journal Article
Published: 01 November 2007
Journal of Paleontology (2007) 81 (6): 1241–1256.
...J. KEITH RIGBY; GORDEN L. BELL, JR.; KIRSTEN THOMPSON Abstract A small faunule of silicified hexactinellid sponges and root tufts has been recovered from the upper Guadalupian Reef Trail Member of the Bell Canyon Formation, from the Patterson Hills, in the southwestern part of the Guadalupe...
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Journal Article
Published: 01 May 2011
Bulletin de la Société Géologique de France (2011) 182 (3): 221–230.
...Jean-Pierre André; Yves Barthet; Michelle Ferrandini; Jean Ferrandini; Jean-Yves Reynaud; Bernadette Tessier Abstract The wide outcrops along the cliffs of Bonifacio at the southern tip of Corsica expose two stratigraphic series of shallow marine deposits, the reefal Cala di Labra Formation (Upper...
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Series: Geological Society, London, Special Publications
Published: 01 January 2001
DOI: 10.1144/GSL.SP.2001.187.01.20
EISBN: 9781862394353
... in the west. For the formation of this ocean–continent transition, four models were proposed after ODP Leg 149. Krawczyk et al. (1996) proposed exhumation of subcontinental mantle accommodated by at least two detachment faults dipping oceanwards, away from Iberia. Brun & Beslier (1996) assumed...
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Journal Article
Published: 01 July 2003
Journal of Paleontology (2003) 77 (4): 674–690.
..., the Pioche Formation was also deposited in a position on the seaward margin of the carbonate platform ( Garcia-Bellido Capdevila and Conway Morris, 1999 ). Modes of preservation in Burgess Shale and similar faunas has been analyzed by such authors as Whittington (1985) , Butterfield (1990) , Briggs...
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Series: Economic Geology
Published: 01 January 2005
DOI: 10.5382/AV100.07
EISBN: 9781934969519
... diamonds (e.g., Pidgeon et al., 1989 ), based on the argument that Archean geothermal gradients were too hot for diamond formation. Detrital diamonds of the Paleoproterozoic Birimian (ca. 2.2 Ga) appear to be the source of most of the alluvial production in Ghana ( Janse and Sheahan, 1995 ), and those...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2017
GSA Bulletin (2017) 129 (5-6): 625–648.
... charnockite massifs and in lowlands along the Palghat-Cauvery shear system, where they are associated with suites of migmatite gneisses, mafic granulites, and metasedimentary rocks (quartzite, banded iron formation, metapelite, calc-silicate, marbles), and mafic-ultramafic intrusives, including chromitite...
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Journal Article
Journal: Economic Geology
Published: 01 June 2007
Economic Geology (2007) 102 (4): 611–631.
..., differentiated volcanic succession composed of two main formations: the ca. 2700 Ma Hébécourt Formation and the 2701 to 2698 Ma Bousquet Formation, which corresponds to the uppermost segment of the Blake River Group. The Hébécourt Formation is composed of regionally extensive LREE-depleted ([La/Sm] N ∼0.9...
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Image
1  Globorotalia (Truncorotalia) broedermanni  Cushman &amp; Bermudez, 1949 ...
Published: 01 January 2014
Figure 4 1 Globorotalia (Truncorotalia) broedermanni Cushman & Bermudez, 1949 , holotype, middle Eocene, Capdevila Formation, Havana Province, Cuba. 2 Globorotalia broedermanni lodoensis Mallory, 1959 , holotype, lower Eocene, lower part of Lodo Formation, Kern County, California. 3
Image
1  Globorotalia (Truncorotalia) broedermanni  Cushman &amp; Bermudez, 1949 ...
Published: 01 January 2014
Figure 4 1 Globorotalia (Truncorotalia) broedermanni Cushman & Bermudez, 1949 , holotype, middle Eocene, Capdevila Formation, Havana Province, Cuba. 2 Globorotalia broedermanni lodoensis Mallory, 1959 , holotype, lower Eocene, lower part of Lodo Formation, Kern County, California. 3