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Bravo Dome

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Journal Article
Published: 01 April 2011
Journal of Sedimentary Research (2011) 81 (4): 248-265.
... hydrothermal origin, just predating migration of mantle-derived gas into the Bravo Dome reservoir. These findings offer insight into questions about the climate significance of dolomite in paleosols, origin of dolomite in hydrothermally altered hydrocarbon reservoirs, and the long-term effect of CO 2...
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A: Map of <b>Bravo</b> <b>Dome</b> gas field (New Mexico, USA), showing top of CO 2 -host...
in > Geology
Published: 23 August 2017
Figure 1. A: Map of Bravo Dome gas field (New Mexico, USA), showing top of CO 2 -hosting Tubb Formation (black contour lines, in m above sea level [a.s.l.]), gas-water contact (short dashed line), the 3 He/ 4 He ratio (long dashed line), and 26 sampling wells (circles). B: West-east cross
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A)  84 Kr&#x2F; 36 Ar plotted against  20 Ne&#x2F; 36 Ar for <b>Bravo</b> <b>Dome</b> samples, comp...
Published: 01 January 2013
Figure 7 A) 84 Kr/ 36 Ar plotted against 20 Ne/ 36 Ar for Bravo Dome samples, compared with air (dotted gray line), air-saturated water (ASW, solid gray line) and the calculated mantle-derived and groundwater end-members, redrawn from Dubacq et al. (2012) . The trends in the concentration
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Location map of wells in the <b>Bravo</b> <b>Dome</b> study region in northeastern New Me...
Published: 01 April 2011
Figure 4 Location map of wells in the Bravo Dome study region in northeastern New Mexico, with studied wells highlighted (modified from Kessler et al. 2001 ).
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Location map of wells in the <b>Bravo</b> <b>dome</b> region with studied wells highlight...
Published: 01 September 2001
Figure 3 Location map of wells in the Bravo dome region with studied wells highlighted (bold dots). The table insert lists names and locations of studied wells. The line linking the study wells is the trace of the fence diagram in Figure 4 .
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Graphic column of paleosols recognized in the <b>Bravo</b> <b>dome</b> study area. Clay-m...
Published: 01 September 2001
Figure 9 Graphic column of paleosols recognized in the Bravo dome study area. Clay-mineral and dolomite content are plotted by intensity, or peak height, in counts per second as recorded by XRD analysis. Magnetic susceptibility is reported as averaged, drift-corrected susceptibility in volume
Journal Article
Journal: Geology
Published: 01 January 2017
Geology (2017) 45 (1): 47-50.
... in the United States are commonly underpressured, suggesting that natural processes reduce the pressure buildup over time and increase storage security. To identify these processes, we studied Bravo Dome natural CO 2 reservoir (New Mexico, USA), where the gas pressure is up to 6.4 MPa below the hydrostatic...
Journal Article
Journal: Geology
Published: 23 August 2017
Geology (2017) 45 (11): 995-998.
...Figure 1. A: Map of Bravo Dome gas field (New Mexico, USA), showing top of CO 2 -hosting Tubb Formation (black contour lines, in m above sea level [a.s.l.]), gas-water contact (short dashed line), the 3 He/ 4 He ratio (long dashed line), and 26 sampling wells (circles). B: West-east cross...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 1992
GSA Bulletin (1992) 104 (7): 802-813.
... shifts during this cycle. Topography related to Early Cretaceous tectonic activity on crystalline basement structures, including the Dalhart Basin, Tucumcari Basin, and the intervening Bravo Dome, also had a direct effect on Early Cretaceous deposition and is reflected by thickness trends in marine...
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2402(06)
... of the cinder cones, lava domes, and related products of the Valle de Bravo Volcanic Field (Fig. 2) . By using geomorphologic parameters of the volcanic structures that formed this field, we determined the different ages of these structures, principally cinder cones, and defined the age range of them...
Journal Article
Published: 01 September 2001
Journal of Sedimentary Research (2001) 71 (5): 817-832.
...Figure 3 Location map of wells in the Bravo dome region with studied wells highlighted (bold dots). The table insert lists names and locations of studied wells. The line linking the study wells is the trace of the fence diagram in Figure 4 . ...
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Series: AAPG Special Publication
Published: 01 January 1951
DOI: 10.1306/SV27345C25
EISBN: 9781629812472
... Abstract The area of the Plainview basin is about 32,000 square miles. It is located between the outcrops of pre-Cambrian rocks in northeast New Mexico on the west, the Bravo dome and Amarillo uplift on the north, and the Matador trend of uplifts on the south. The belt of uplifts along...
Journal Article
Journal: Geosphere
Published: 01 February 2015
Geosphere (2015) 11 (1): 160-184.
... faults such as the Acambay fault, which moved during the 1912 Acambay earthquake, or the Venta de Bravo fault. A relatively large slip rate estimated for this fault branch (0.23–0.37 mm/yr) leads us to contemplate the possible connection at depth between the Pastores and the Venta de Bravo faults...
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Journal Article
Published: 01 June 2006
Canadian Journal of Earth Sciences (2006) 43 (5): 593-616.
...Shannon M. Johns; Herwart H. Helmstaedt; T. Kurtis Kyser Abstract Rocks of the Bravo Lake Formation on Turtle Back Island and Pillow Island off the western coast of central Baffin Island, Nunavut, represent a well-exposed example of the mafic volcanic and intrusive sequences commonly preserved near...
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Series: AAPG Special Publication
Published: 01 January 1926
DOI: 10.1306/SV1328C22
EISBN: 9781629812601
... Abstract Although the salt has not been drilled into, the presence of a typical cap-rock mass of anhydrite and gypsum capped by “lime” rock indicates that Saratoga is a salt dome. The cap rock is elliptical in plan with its major axis about 1½ miles in length and northeast-southwest in strike...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1925
AAPG Bulletin (1925) 9 (2): 263-285.
... the anhydride is taken as the top of the dome. This surface is irregular and in some instances might take in sandstone layers which have become cemented with lime. There is evidence that the limestone cap is thicker in the center of the dome than on the edges. Well No. 332 Cotton, of the Rio Bravo Oil Company...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2014
GSA Bulletin (2014) 126 (11-12): 1625-1653.
... and Archean gneiss domes located immediately to the south ( Fig. 2 ; Snyder, 2003 ) is consistent with significant thinning of the lithosphere during Bravo Lake formation magmatism. These discontinuities have been interpreted to reflect Archean mantle lithospheric thinning associated with Paleoproterozoic...
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Journal Article
Journal: GSA Bulletin
Published: 01 October 2001
GSA Bulletin (2001) 113 (10): 1324-1342.
... plagioclase and hornblende; this dacite forms clusters of steep-sided domes or widespread pyroclastic deposits, and the latest eruptions, dated by radiocarbon and K-Ar, occurred between 0.03–0.05 Ma. Estimates of the volume of magma erupted in the Zitácuaro–Valle de Bravo region in the past 1 m.y. (1.8 km 3...
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Series: AAPG Memoir
Published: 01 January 1975
DOI: 10.1306/M6382C14
EISBN: 9781629812120
... on the flanks ofknown plugs and deeper drilling in two fieldswhich were believed to be domes, although salthad not been reached. The Texas, Gulf, Humble, Rio Bravo(Southern Pacific), and Sun companies, whichhad acquired ...
Series: Geological Society, London, Memoirs
Published: 01 January 2014
DOI: 10.1144/M39.25
EISBN: 9781862396821
... evacuations in the absence of dome growth was a problem again in 2007, when there was a large, but (apparently) silent, dome over the NW. The BGS was very sensitive about legal issues and, given the presence of high uncertainty, was keen not to take any risks at all (for details of the BGS’ legal troubles...
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