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Campil Member

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Sedimentary facies of the <b>Campil</b> <b>Member</b> within the study area.
in > PALAIOS
Published: 01 April 2016
Table 1.— Sedimentary facies of the Campil Member within the study area.
Journal Article
Journal: Geology
Published: 01 May 2004
Geology (2004) 32 (5): 461–464.
... , Rhizocorallium , Planolites , and Gyrochorte that indicate a subtidal paleoenvironment. Wrinkle structures were found in the Campil Member in the Werfen Formation of northern Italy and in the Virgin Limestone Member of the Moenkopi Formation and the upper member of the Thaynes Formation exposed in the western...
FIGURES
Journal Article
Journal: PALAIOS
Published: 01 April 2016
PALAIOS (2016) 31 (4): 161–176.
...Table 1.— Sedimentary facies of the Campil Member within the study area. ...
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Journal Article
Journal: Geophysics
Published: 25 June 2015
Geophysics (2015) 80 (4): KS51–KS68.
... methods for the detection of small changes. In between these two end-member cases, there are the presently discussed results: spatially variable ε estimates observed together with more or less strong d c episodes indicate medium changes that are characterized by variations in the elastic...
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Journal Article
Published: 01 May 2007
Journal of Paleontology (2007) 81 (3): 415–434.
... Bu-54) were collected from the Siusi Member, “transitional facies,” and Campil Member of the Werfen Formation at the Bulla section, precisely following the sample numbering scheme of Farabegoli and Perri (1998) . Samples above Bu-26 are not shown in Figure 2 , however, because they were barren...
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Image
Figure 1. Late Permian–Early Triassic paleogeographic map (modified from  E...
in > Geology
Published: 01 May 2004
, Spathian Virgin Limestone Member, Moenkopi Formation; (2) western United States, Spathian upper member, Thaynes Formation; (3) northern Italy, Smithian Campil Member, Werfen Formation
Image
Figure 3. Photographs of Cambrian and Early Triassic wrinkle structures for...
in > Geology
Published: 01 May 2004
Figure 3. Photographs of Cambrian and Early Triassic wrinkle structures for comparison. A: Lower Cambrian Poleta Formation, Westgard Pass, central California, United States (37°17′30″N, 118°08′00″W). B: Smithian Campil Member, Werfen Formation, Punta Rolla locality, northern Italy ( Broglio Loriga
Journal Article
Journal: PALAIOS
Published: 01 June 2005
PALAIOS (2005) 20 (3): 213–223.
... stratigraphy and correlation from Twitchett (1999 and references therein). Nevada stratigraphy and correlation from Schubert and Bottjer (1995) . U. Perm = Upper Permian. TOH = Tesero Oolite Horizon Asteriacites lumbricalis are most common in the Campil Member (Smithian), and have been found...
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Series: Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.228.01.18
EISBN: 9781862394766
.... The sediments record deposition in a mixed carbonate-siliciclastic environment above storm wavebase and below fair-weather wavebase. Both preevent and post-event ichnofaunas are present, and benthic conditions were clearly improving. The overlying Smithian age Campil Member, however, records a temporary...
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Book Chapter

Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/SR24.13
EISBN: 9781862396920
... on these diverse faunas. Within the overlying Campile Formation, the Garraun, Newtown Head and Ross members have been recognized. Higher in the succession, the Raheen shales occur within the upper part of the Campile Formation or possibly above it. Diverse upper Caradoc trilobite ( Owen et al. 1986...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.182.01.16
EISBN: 9781862394308
.... Productivity bar charts for Regionally Important Aquifers (a) Quaternary deposits, (b) Wexford Limestone Formation, (c) Campile Formation, (d) Kiltorcan Sandstone Formation. The Geological Survey of Ireland (GSI) has created a system of aquifer classification for use in groundwater protection...
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Journal Article
Journal: Geology
Published: 01 July 2000
Geology (2000) 28 (7): 643–646.
... Triassic Werfen Formation (basal oolitic Tesero horizon and the overlying Mazzin, Seis, and Campil Members) ( Holser and Schönlaub, 1991 ) (Fig. 1) . The upper 57 m in the core consists of Middle Triassic Muschelkalk conglomerate; interbedded ash-flow tuff is present from 30 to 34 m. Dolomitization...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.1
EISBN: 9781862393899
... area in the southwestern part of the Transdanubian Range ( Broglio Loriga et al. 1990 ). In the Western Dolomites, the Upper Permian is made up of the evaporitic/dolomitic Fiamazza fades of the Bellerophon Formation that is overlain by the oolitic grainstone/packstone of the Tesero Member...
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Journal Article
Published: 01 February 2016
Mineralogical Magazine (2016) 80 (1): 157–174.
...-water and magma-sediment interaction, which will provide evidence of heat energy and fluid mobility in a potential mineralizing system. Mineral alteration assemblages are investigated particularly near the interface between magmatic and sedimentary end members within peperite, in order to isolate ocean...
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Journal Article
Published: 03 August 2015
Geological Magazine (2016) 153 (2): 271–284.
... successions of the Hungarian Transdanubian Range. The inputs of illite–smectite, smectite and variable kaolinite observed, especially in the Menschely Marl Member, were taken by Rostasi Rausick & Varga ( 2011 ) as evidence for more humid hinterland climates during...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 March 2019
Economic Geology (2019) 114 (2): 207–232.
... ). Abbreviation: HMC = heavy mineral concentrate. The bedrock geology of North Wexford is similar to that of southern Wicklow, although the Avoca Volcanic Group is not represented in Wexford. Duncannon Group metasediments and volcanic rocks, constituting the Campile Formation, form a northeast-southwest...
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Journal Article
Published: 01 December 1990
Journal of the Geological Society (1990) 147 (6): 1035–1050.
.... During the Early Ordovician the basin became more extensive, so that Ribband deposition became more widespread. After minor tectonic activity the basin shallowed in the Upper Ordovician so that shelf carbonates of the Duncannon Group were deposited, with local unconformity, on various members of the 1035...
Journal Article
Published: 01 February 2004
Journal of Paleontology (2004) 78 (2): 300–316.
... ( Jurkovsek, 1983 ); ?Italy: Lucania (Apennine), M. Facito Formation, ‘terrigenous' Member, in association with D. (A.) taramellii , D. (Moussonella) udvariensis and D. boeckhi ; Fassanian ( De Capao Bonardi, 1969 ); ?Romania: Bukowina (Pdealul Cailor, Piatra Zimbrului), Ladinian ( Turculet, 1972...
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