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Fort Bowie Fault

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Journal Article
Journal: GSA Bulletin
Published: 13 November 2024
GSA Bulletin (2024)
... of an originally sub-horizontal thrust fault, the Fort Bowie fault, and a thin-skinned ramp-flat thrust system that is offset by a younger thrust fault, the Apache Pass fault, that carries basement rocks. Cross-cutting relationships and new geochronologic data indicate deformation on both faults occurred between...
Journal Article
Journal: GSA Bulletin
Published: 01 October 1957
GSA Bulletin (1957) 68 (10): 1315–1342.
... the Emigrant fault cut the autochthonous block and the overlying thrust sheet, which was separated into the Fort Bowie plate and the Wood Mountain plate. The Fort Bowie plate was later folded to form the Marble Quarry syncline and was truncated by the younger Fort Apache reverse fault. Finally, the Whitetail...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1951
AAPG Bulletin (1951) 35 (6): 1274–1293.
... of the Muenster arch is exceedingly steep due to extensive faulting and plunges off 7,500 feet or more into the Fort Worth basin within a few miles. The northeastern limb is relatively gentle until within a few miles of the axis of the Marietta-Sherman syncline where steep dips and extensive faulting are likewise...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1953
AAPG Bulletin (1953) 37 (6): 1416–1430.
..., indicating disappointingly small reserves. New producing strata were located at Fort Trinidad, Douglass, Pine Mills, West Waskom, Elysian fields, and Yantis fields. Drilling operations in proved areas continued to decline in 1952. The East Texas field was the most active field, by a narrow margin. Total...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1945
AAPG Bulletin (1945) 29 (6): 766–776.
.... © 1945 American Association of Petroleum Geologists. All rights reserved 1945 American Association of Petroleum Geologists The East Texas district is essentially the East Texas basin, and extends from the Fort Worth basin on the west, to the Louisiana state line on the east. North and south...
FIGURES
Journal Article
Published: 01 June 1964
Jour. Geol. Soc. India (1964) 5 (1): 112–120.
...: Torbernite, autunite, and infrequent specks of pitchblende occur in the old copper workings at Kho-Daribo, where mineralisation is localized in the north-westerly high-angle faults in the strongly folded phyllites, biotite-schists and arkosic quartzites. The presence of chalcopyrite, pyrrhotite, cubanite...
Journal Article
Journal: GSA Bulletin
Published: 04 November 2024
GSA Bulletin (2024)
... moderate high-Y rims. Geological Society of America Bulletin, v. 136, no. XX/XX 13 Bowie et al. Figure 8. Summary of calculated pressure-temperature (P-T) conditions. Top: schematic cross section illustrates relative structural position of analyzed samples between the Okanagan Valley fault system...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1943
AAPG Bulletin (1943) 27 (6): 782–789.
... the Association at Fort Worth, April 7–9, 1943. Manuscript received, May 17, 1943. 2 Trowbridge Sample Service, Owen Building. 3 Humble Oil and Refining Company. © 1943 American Association of Petroleum Geologists. All rights reserved 1943 American Association of Petroleum Geologists...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1965
AAPG Bulletin (1965) 49 (6): 749–765.
... by a fault closure. Three other producing wells have been completed, and one dry hole has been drilled. Table IV. PRODUCTION IN EAST TEXAS, 1963–1964 Table V. WELL COMPLETION SUMMARY, 1964 Thirty-four tests were drilled to the Jurassic Smackover, one less than in 1963. There were...
FIGURES | View All (5)
Journal Article
Published: 01 February 1992
Bulletin of the Seismological Society of America (1992) 82 (1): 454–480.
... the 1857 earthquake and plate tectonic loading. The postseismic displacements have been calculated using a elastic / viscoelastic coupling model that, for any fault geometry, yields the exact displacements on a spherically stratified Earth. The southern California crust and upper mantle are modeled...
Journal Article
Published: 01 October 2007
Earth Sciences History (2007) 26 (2): 229–261.
... having a diameter of about half that of the Earth. The difference between the final corrected gravity value for a station and the theoretical value predicted by the spheroid model used (see Part I), gave what came to be called the free-air anomaly or the Bouguer anomaly (Hayford and Bowie 1912, p...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1957
AAPG Bulletin (1957) 41 (3): 466–510.
... Quadrangle and south of Bowie Mountain, where it is strongly faulted. The outcrops in Secs. 28 and 29, T. 16 S., R. 30 E., have been recrystallized by contact metamorphism. There are outcrops at Blue Mountain, Wood Mountain, and Dunn Springs Mountain. At the last two places, the Horquilla forms the sole...
FIGURES | View All (15)
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1935
AAPG Bulletin (1935) 19 (2): 153–171.
... alternating with rubbly and highly argillaceous strata. 11 The following summarized log of a well at Fort McMurray gives further information regarding the Devonian: 12 Feet   0–40 Overburden 40–415 Limestones and shales 415–782 Limestones and shales, with anhydrite, gypsum...
FIGURES
Journal Article
Published: 01 April 1995
Earth Sciences History (1995) 14 (1): 62–83.
... is still hung up over the proper attitude toward Wegener. In an editorial “Geological Science in Its Decadence?” he includes the mobilist heretics in his pantheon of brilliant theorists: Davis and Daly of Harvard, Lawson of Berkeley, Chamberlin of Chicago, Reid and Berry of Johns Hopkins, Taylor of Fort...
Journal Article
Published: 01 September 1927
Bulletin of the Seismological Society of America (1927) 17 (3): 149–182.
.... This article is briefly reviewed in Zeitschrift fiir Geophysik, 1, Heft 6, 262, 1924-1925. 6. BowIE, WiLLIAZVg"Notes on the Airy or 'Roots of Mountains' Theory," Scie~zee, No. 1632, 63, 371-374, April 9, 1926. 7. BRAND, JOI~ANN, "Ein Beitrag zum Stadium der Bodenbewegungen nicht seismischen Ursprungs...
Journal Article
Published: 01 March 1927
Bulletin of the Seismological Society of America (1927) 17 (1): 25–48.
... from the Fort Tejon earthquake of 1857. It is characteristic of these features that they change abruptly from place to place along the strike of the fault Within half a mile a scarp may give place to a ridge and the ridge to a trough ; or a scarp facing REPORT OF THE ADVISORY COMMITTEE IN SEISMOLOGY 27...
Journal Article
Published: 01 October 1994
Earth Sciences History (1994) 13 (2): 143–153.
... to the geology of Texas: 1. They advanced the knowledge of the State’s Cretaceous rocks, even though they did not recognize the Balcones Fault Zone and arranged part of the section erroneously; 2. They determined that not all mountains in the Southwest were formed around granite cores; and 3. They discovered...
FIGURES | View All (6)
Journal Article
Published: 01 December 1922
Bulletin of the Seismological Society of America (1922) 12 (4): 199–219.
.... In another paper I have presented evidence, partly geologic but largely physiographic or seismologic, which indicates (1) that the east-west arcs delineating the major relief features of the Greater Antilles are zones of normal faulting developed in late geologic time; (2') that this faulting has resulted...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1935
AAPG Bulletin (1935) 19 (10): 1508–1537.
... at the foot of the Highlands” and “Beds of the Highlands” with what is now known as the Balcones fault scarp as the basis for the division. Roemer regarded the beds forming the escarpment as younger than those at its foot. This error is easily understood in the light of history by the fact that at that time...
FIGURES | View All (10)
Journal Article
Published: 01 June 1916
Bulletin of the Seismological Society of America (1916) 6 (2-3): 55–180.
... from the coast, east of Fort Ross, the Mount St. Helena fault follows a NW.-SE. direction for more than twenty miles along the southwest base and flank of the mountain. Though it is not a very satisfactory procedure to correlate shocks definitely with this, nevertheless it is a possible locus of origin...