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Newtown Fault

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Series: SEPM Special Publication
Published: 01 January 2007
DOI: 10.2110/pec.07.87.0193
EISBN: 9781565762954
... of Gorge-1. The excavation of the Gorge revealed waterflow through rectilinear dissolution-enlarged fractures, joints, and faults. The jointing in this bed is well developed compared tomost of the rest of the section. We attribute this to the dolomitemineralogy resulting in different rock properties...
Journal Article
Published: 01 March 1986
Journal of the Geological Society (1986) 143 (2): 327-334.
... vertical faults. First motion data for both 1984 events also give a nodal plane in this orientation. In the first case, the event can be clearly attributed to mapped N-S vertical faults SE of Newtown, and in the second, a deep N-S normal fault under the Lleyn Peninsula is inferred as the most likely fault...
Journal Article
Published: 01 June 2019
South African Journal of Geology (2019) 122 (2): 117-142.
... of the current study. The Swartklip Sector extends from slightly north-east of the Crocodile River fault in the north to a few kilometers south of the Pilanesberg in the south, but for practical purposes this contribution refers only to that portion north of the Pilanesberg ( Figure 1 ). There are three...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 2001
AAPG Bulletin (2001) 85 (12): 2061-2087.
... ). Although no evidence of middle-Late Permian faulting is seen in central Spitsbergen, variations in accommodation on Svalbard generally reflect the distribution of earlier structural elements, and Dickson Land lies within the Nordfjorden structural block, which was a persistent positive feature...
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Journal Article
Published: 01 January 2002
Journal of Sedimentary Research (2002) 72 (1): 95-115.
... to the Nordkapp basin. The same platform strata are believed to continue eastward through the disputed boundary zone with Russia (long dashes) and thence southeastward along the Kola Monocline. The fault-bounded Nordkapp Basin contains thick salt deposits believed to have formed during relative sea-level...
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Series: Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.239.01.11
EISBN: 9781862394872
... of the geological modelling issues, is topical. The integrity of an underground waste repository in this environment is threatened by a number of geological processes and events, including earthquake activity and active faulting, active volcanism and geothermal activity, uplift, erosion and other natural phenomena...
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Journal Article
Journal: Clay Minerals
Published: 27 May 2019
Clay Minerals (2019) 54 (2): 181-196.
...Simon J. Kemp; Martin R. Gillespie; Graham A. Leslie; Horst Zwingmann; S. Diarmad G. Campbell Abstract Temporary excavations during the construction of the Glendoe Hydro Scheme above Loch Ness in the Highlands of Scotland exposed a clay-rich fault gouge in Dalradian Supergroup psammite. The gouge...
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Journal Article
Published: 01 November 1984
Journal of the Geological Society (1984) 141 (6): 1001-1014.
...N. H. Woodcock Abstract The NE-trending Pontesford Lineament centres on the Pontesford-Linley and adjacent faults in the Shelve/Longmynd inlier. To the NE it is usually drawn along the SE edge of the Cheshire Basin and to the SW along a variety of lines parallel to or converging with the Church...
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.180.01.07
EISBN: 9781862394285
... in Argyll. The rocks are believed to represent an intermontane alluvial fan environment. The sediments occur in an outcrop of 3 km length against the northern flank of Knockalla Mountain, bounded to the southeast by the NE–SW-trending Caledonian Leannan Fault and resting on fractured Argyll Group Dalradian...
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Journal Article
Published: 01 May 2012
Proceedings of the Yorkshire Geological Society (2012) 59 (1): 37-51.
...) Simplified pre-Carboniferous stratigraphy and basement geology of Charnwood Forest showing the Groby study area (modified from Carney 1999 ). NP, New Plantation; GP, Groby Pool; SP, Stable Pit; DP, Deer Park Spinney; NLF, Newtown Linford Fault. Despite the extent of this younger cover...
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Journal Article
Journal: Economic Geology
Published: 01 January 2003
Economic Geology (2003) 98 (1): 31-50.
...C. E. Everett; D. M. Rye; R. M. Ellam Abstract The Zn-Pb (-Ba) deposits of central Ireland are hosted by Lower Carboniferous Waulsortian limestone and Navan Group carbonate sediments. The deposits are located near the margins of subbasins in close association with extensional faults. The source...
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Published: 06 October 2006
DOI: 10.1130/2006.fld008(06)
EISBN: 9780813756080
... Faults), Mount Cuba Wissahickon (south and east of the Street Road fault, including a strip immediately east of the Wilmington Complex), and Wissahickon Formation (sensu stricto) (east of the Wilmington Complex). Day 1 treats the rocks north of the Martic Line. Day 2 addresses rocks south of the Martic...
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Image
Regional setting of the study area.  (A)  Location map of Charnwood Forest ...
Published: 01 May 2012
stratigraphy and basement geology of Charnwood Forest showing the Groby study area (modified from Carney 1999 ). NP, New Plantation; GP, Groby Pool; SP, Stable Pit; DP, Deer Park Spinney; NLF, Newtown Linford Fault.
Journal Article
Published: 01 May 2005
Quarterly Journal of Engineering Geology and Hydrogeology (2005) 38 (2): 223-224.
... section, entitled ‘Urban Areas’, presents accounts of the natural geology encountered in a number of urban centres, but not all. Cardiff, Bangor and Newtown are included, but Aberystwyth, Bridgend, Newport, and Rhondda are not. However, it is understood that a second volume is being planned...
Journal Article
Published: 01 April 2007
Mineralogical Magazine (2007) 71 (2): 235-240.
... in this geothermal field, in an area located ~6 km to the NE of Copahue Volcano. These wells confirm the presence of a vapour-dominant type reservoir at a depth of more than ~800 m. The four wells constitute an area of 1 km 2 , located on a WNW–ESE fault system that links the Chancho Co geothermal centre in Chile...
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Journal Article
Published: 01 June 1989
Journal of the Geological Society (1989) 146 (3): 417-418.
... units, the Clammers Point and Wexford units, by the Ballymadder fault. The lithostratigraphy and proposed correlation between these units is illustrated in Fig. 1. The Kiln Bay, ~ ~ ~~ ~~ ~ SOUTHEAST IRELAND. CAHORE GROUP Cl ammers Point Unit. Wexford Unit t AROENAGH FORMATION. CULLENSTOWN FORMATION...
Journal Article
Published: 01 April 1974
Journal of the Geological Society (1974) 130 (2): 157-161.
... Palaeozoic volcanic belts of South East Ireland. Abstr. VIII Int. Sed. Congr. Heidelberg 1971 88 Seilacher A. Fault graded beds interpreted as seismites Sedimentology 1969 13 155 Stillman C. J. Ordovician ash-fall tuffs from Co Waterford Sci Proc R Dubl Soc 1971 4A 89...
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR25.12
EISBN: 9781862396937
... sedimentary structures, the direction of slumping, the mineralogy and the nature of the trace fossils all point to deposition of the sediments in a fault-controlled subsiding marine basin, the Leinster Basin, west of the Rosslare/ Monian Terrane. As discussed in Chapter 11 of this report, some authors...
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Journal Article
Published: 01 February 1999
Journal of the Geological Society (1999) 156 (1): 73-87.
.... A geophysical survey of Poole Bay to trace a palaeoriver valley from Poole Harbour. MSc Dissertation, Department of Oceanography, Southampton University. Dean, J.M. 1995. Holocene palaeo-environmental reconstruction for the nearshore Newtown Area, Isle of Wight. BSc Dissertation, Department...
Journal Article
Journal: Geosphere
Published: 11 December 2019
Geosphere (2019)
... of Ganderia, called the Red Indian Line, remains an open matter of debate (Dorais et al., 2012; Macdonald et al., 2014, 2017; Coish et al., 2015; Tremblay and Pinet, 2016; Karabinos et al., 2017). The Red Indian Line, defined in New- foundland, is a major terrane-boundary mylonitic fault that separates rocks...