... features of the region. This correlation suggests that the tectonic setting of the Charleston region is controlled by scissors- like compression on a crustal block located between the north-trending Adams Run fault and the northwest-trending Charleston fault. Tectonism is localized in the Charleston region...

... occurred in shales at 480 and 1,040 feet below the Top Hard level. It is in a basin area disturbed by faults of moderate size. West Drayton, Nottinghamshire .—In a coal boring at West Drayton, 3 miles north of Tuxford, a thin-bedded sandy mudstone was encountered at 3,161 feet, at the horizon...

...Figure 5. ▴ A) Overlay of the Drayton limestone valley (dashed contours) and Fort Bull dome (gray pattern) with the WF offset model of Talwani and Durá-Gómez ( 2009 ). B) Overlay of domes and areas of proposed uplift (gray areas modified from Marple and Talwani 2000 and Weems and Lewis 2002...

... , G. W. , 1969 , Geological developments in the eastern Officer basin of South Australia : Australian Petroleum Exploration Assoc. Jour. , v. 9 , no. 2 , p. 8 – 13 . Laherrere , J. , and R. D. Drayton , 1965 . Some geophysical results across the Simpson desert : Australian...

... Mountain region. Oil was discovered in the Cambrian Deadwood sand in the Lost Soldier field in the Drayton well No. 2, completed on June 26, 1948, at 5,965–6,130 feet, initially producing 720 barrels per day, flowing by gas lift. A second well (No. 111A) was completed in December, 1948, flowing 601...

... NEWFOUNDLAND, CANADA: POSSIBLE IMPLICATIONS FOR HYDROCARBON EXPLORATION N.A. YASSIR Department of Earth Sciences University of Waterloo Waterloo, Ontario N2L 3G1 A.L. ROGERS Mobil Oil Canada Box 150 Drayton Valley, Alberta TOE OMO INTRODUCTION Issler's concern with our paper (see Issler, 1994, this issue...

... Drayton horst. Syn-sedimentary normal faults of Permo-Triassic age developed as a result of, and detach onto, a putative re-actived Variscan compressional structure (thrust). Note in this area, the major thickening of the Sherwood Sandstone Group and Permian formations appears to occur across a fault...

... this tectonic high ( Figs. 4 , 9A ). The Mount Forest valley extends from Mount Forest to Drayton for 35 km in the Salina Formation, and, despite an extremely undulating longitudinal profile, it has a gradient to the southeast ( Fig. 8C ). This valley not only differs from the broad Walkerton trough...

... in the basal Permain sandstones below the mark (Collyhurst Sandstone). These changes (from 0-330 m in lOO0m laterally) have been cited as evidence (Tonks et al. 1931, p. 162) to demonstrate contemporaneous faulting 1993, pp. 857-870. with greater thicknesses of aeolian sand apparently occurring...

.... The highest simulated groundwater heads above ground surface occur in the north of the groundwater model (Market Drayton–Wellings groundwater management unit). It appears that this is because the model does not have a sufficient coverage of stream boundaries to allow enough stream discharge in this area...

... at Pinopolis along the peninsula in Lake Marion to the northeast all suggest continuous seismicity on the Woodstock fault (N) (A.18, Figure 14A ). The rupture of the north and south walls of the Drayton family tomb on the grounds of the Magnolia Plantation along a northwest trend suggest movement...

...Kiran Kumar Singh Thingbaijam; Mark S. Rattenbury; Russ J. Van Dissen; Matt C. Gerstenberger; John Ristau; Delphine D. Fitzenz Abstract Applying distributed seismicity models for seismic hazard analysis requires postulating the styles of faulting and nodal planes for anticipated earthquakes. Here...

...Nigel E. Cross; Zana K. Williams; Arman Jamankulov; Candice E. Bostic; Valini C. Gayadeen; Helisaul J. Torrealba; Elizabeth S. Drayton ABSTRACT The Pliocene reservoirs of the North Coast Marine Area (block NCMA-1) comprise shallow marine shoreface to shelf sandstones (up to 30 m [98 ft] thick...

... , doi: 10.1144/1354-079304-638 . Ainsworth R. B. , 2006 , Sequence stratigraphic-based analysis of reservoir connectivity: Influence of sealing faults—A case study from a marginal marine depositional setting : Petroleum Geoscience , v.  12 , p.  127 – 141 , doi: 10.1144/1354-079305-661...

... track damage in 1886. Red dots on the railroads show locations specific damage (flexures, cuts), and red dashed lines show the approximate orientations of notable “fissures” formed in 1886. Blue dots show earthquake epicenters. Heavy red lines denote Gants (G), Cooke (Co), and Drayton (Dr) faults...

.... Northernmost of the target sub-catchments, the Upper Wylye lies to the north of the Mere Fault in a large block of Cretaceous units including the Upper Greensand, Gault Clay and Chalk. The sub-catchment covers an area of 70 km 2 upriver of Hill Deverill, adjacent to the village of Longbridge Deverill ( Fig. 2...