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Saint Clair Fault

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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1979
AAPG Bulletin (1979) 63 (4): 647–654.
..., the base of the Rome at 28 ft (8.5 m) in the Strader well is marked by a major thrust fault. We have interpreted this thrust as part of the Saint Clair fault system and attribute the formation of the Bane dome to imbrication at the trailing edge of the Saint Clair footwall. The subsurface data refute...
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Journal Article
Published: 01 May 2003
American Mineralogist (2003) 88 (5-6): 837–845.
...Claire-Isabelle Fialips; Juraj Majzlan; Daniel Beaufort; Alexandra Navrotsky Abstract The energetics of the Saint Claire dickite sample, a highly pure and low defect material, have been studied by high-temperature oxide-melt solution calorimetry. Data were corrected for adsorbed water, the only...
FIGURES
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 August 2009
Lithosphere (2009) 1 (4): 206–226.
...Sarah Draper Springer; James P. Evans; John I. Garver; David Kirschner; Susanne U. Janecke Abstract The San Andreas Fault Observatory at Depth (SAFOD) drill hole encountered indurated, high-seismic-velocity arkosic sedimentary rocks west of the active trace of the San Andreas fault in central...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2012
AAPG Bulletin (2012) 96 (6): 1147–1169.
... gradient based on apatite fission track studies ( Grist et al., 1992 ; Li et al., 1995 ), and high-temperature fluid inclusions correlated with active faulting in the Jurassic carbonate bank ( Weirzbicki et al., 2006 ). None of these studies were able to well constrain the timing of the thermal event...
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Journal Article
Published: 04 February 2020
Bulletin of the Seismological Society of America (2020) 110 (2): 698–714.
... seismic zone (WQSZ), and the Lower Saint Lawrence seismic zone (LSLSZ) over a depth range of 5–30 km ( Ma and Lamontagne, 2017 ). The CSZ is characterized by northeast–southwest‐trending reverse fault structures and focal mechanisms with northwest–southeast‐striking maximum compressive stresses. The WQSZ...
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Journal Article
Published: 31 May 2019
Canadian Journal of Earth Sciences (2019) 56 (12): 1398–1408.
... (historical and instrumental) with focal mechanisms as extracted from the recently published seismotectonic map of Africa. We identify active transform faults, the Chain (CFZ), Romanche (RFZ), Saint Paul (SPFZ), and Arkhangelskiy (AFZ) fault zones. We also calculate strain rates on these faults from Late...
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Journal Article
Published: 01 January 2013
Bulletin de la Société Géologique de France (2013) 184 (1-2): 155–164.
... and after the event, the upper part slid down along pre-existing faults (named F1, F2 and F3 on fig. 4a ) that frame the head of the eroded cliff. At the bottom, the left and right lateral parts of the cliff were also removed. It is likely that the falling upper part pulled down the lower parts, assisted...
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Journal Article
Published: 18 August 2011
Canadian Journal of Earth Sciences (2011) 48 (9): 1293–1306.
... ) measurements. Inclusions that showed stretching were excluded from the study. Microthermometric measurements of fluid inclusions were performed using a Linkam FTIR 600 heating-freezing stage mounted on an Olympus BX51 microscope (Saint Mary’s University, Halifax, Nova Scotia, Canada). The stage was calibrated...
FIGURES
Journal Article
Published: 01 September 2012
Bulletin de la Société Géologique de France (2012) 183 (5): 409–424.
...Henri Rouvier; Bernard Henry; Maxime Le Goff Abstract Une réaimantation “syntectonique” éocène a été mise en évidence dans toute la virgation des Corbières, des Fenouillèdes à l’arc de Saint-Chinian. Son analyse montre que le synclinorium de Saint-Paul de Fenouillet a conservé son orientation E-W...
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Journal Article
Published: 15 November 2017
Canadian Journal of Earth Sciences (2018) 55 (3): 241–251.
... with a red line. [Colour online.] Fig. 11. A schematic north–south section through the northern margin of the St. Lawrence graben near Sainte-Sophie. We propose that the graben descends in a series of steps, like a staircase, rather than a single fault. The limit between the blocks could also...
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Journal Article
Published: 01 March 2011
Bulletin de la Société Géologique de France (2011) 182 (2): 111–132.
...-window nappe anticline as shown by the 345 m uplift of the l’Escuichière paleo-canyon. The reconstructed paleo-drainage network attests for the tectonic activity of the Barles nappe anticline, the Bès tear fault, the Saint Benoît tear faults and the Digne nappe during the Pliocene and the Quaternary...
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Journal Article
Published: 01 March 1996
Bulletin de la Société Géologique de France (1996) 167 (2): 295–302.
... gneiss domes and detachement fault systems : structure and kinematics" (BRUN J.-P. and VAN DEN DRIESSCHE J., Bull. Soc. géol. Fr., 1994, 165, 6, 519-530) par MICHEL DEMANGE Mots clés: Chaîne hercynienne, Montagne Noire, Dôme de gneiss, Nappes, tectonique d'extension, Métamorphisme, Migmatite Résumé: Le...
Journal Article
Journal: Geosphere
Published: 05 June 2019
Geosphere (2019) 15 (4): 983–1007.
..., respectively, to the western and eastern slope of the islands, calculated between the coast and the slope break at ∼250 mbsl. We also ran models that take into account the fact that the modern Les Saintes plateau is offset by small normal faults. These faults have 5–8-m-high scarps on the plateau, whereas...
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Journal Article
Published: 01 September 2008
Bulletin de la Société Géologique de France (2008) 179 (5): 503–518.
... to the upper crustal section of Trinity, the contact relationships between these lavas and the underlying gabbros and diabase dykes are not preserved, and likely faulted [cf. Brouxel and Lapierre, 1988 , p. 1112]. The main stream of the Trinity river, i.e. the base of our section, corresponds...
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Journal Article
Journal: Geosphere
Published: 09 February 2018
Geosphere (2018) 14 (2): 469–491.
...Hugues Raimbourg; Vincent Famin; Giulia Palazzin; Mathieu Mayoux; Laurent Jolivet; Claire Ramboz; Asuka Yamaguchi Abstract Fossil structures, such as exhumed accretionary prisms, are the only direct recorders of the fluids wetting the plate interface near the base of the seismogenic zone...
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Image
—Cross-sectional model of Giles County, Virginia, showing inferred subsurfa...
Published: 01 April 1979
Fig. 4. —Cross-sectional model of Giles County, Virginia, showing inferred subsurface configuration of Saint Clair fault system. a , Major fault block identified in Strader well; b , second fault slice, inferred to be present beneath Bane dome on basis of constraints of model; c, autochthonous
Journal Article
Published: 01 July 2015
Rocky Mountain Geology (2015) 50 (1): 30–118.
... persisted until late Eocene time. As expected, remnants of basin margins universally show major thinning of stratigraphic sequences. Principal thinning was from tectonic causes, however, exhibiting erosional angular unconformities only rarely. Out-of-the-basin, younger-on-older faulting (in which fault...
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Journal Article
Published: 01 October 1963
Bulletin of the Seismological Society of America (1963) 53 (5): 873–891.
... Risk in the Wellington District , New Zealand Science Review , 14 : 132 - 135 . Whitten C. A. Claire C. N. 1960 . Analysis of Geodetic Measurements along the San Andreas Fault , Bull. Seism. Soc. Amer. 50 : 404 - 415 . Wilt J. W. 1958 . Measured...
Journal Article
Published: 01 January 1949
Bulletin of the Seismological Society of America (1949) 39 (1): 1–8.
.... Geol., 28:1767-1774 (December, 1944). 10Bailey Willis, "Normal Fault Structures and Others," Bull. Am. Assoc. Petr. Geol., 30:1875-1887 (November, 1946). n Stuart Weller and Stuart St. Clair, "Geology of Ste. Genevieve County, Missouri," Mo. Bur. Geol. and Mines, 2d Ser., Vol. 22, 352 pp. 1928. ~ J. M...
Journal Article
Journal: Geosphere
Published: 01 August 2012
Geosphere (2012) 8 (4): 805–834.
... ). The microplate is separated from the North American plate by the Fairweather right-lateral fault to the east, the Aleutian megathrust to the northwest, and the Chugach–Saint Elias thrust to the north ( Fig. 1 ). The Chugach–Saint Elias Range records deformation and exhumation within the zone of convergence...
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