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Surrency bright spot: possible evidence for fluid in the deep crust

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:5951893
New COCORP profiles in eastern Georgia may indicate the presence of trapped fluid and/or gas in the deep crust. The evidence takes the form of an anomalously high amplitude reflection occurring at 6 sec 2-way time (15-18 km depth) on Georgia line 16. This reflection, termed the Surrency bright spot bears a startling resemblance to bright spots that are observed by the petroleum industry in sedimentary sequences, and which are commonly associated with hydrocarbon accumulations. The Surrency bright spot has a very high amplitude, is overlain by a faint anticlinal feature, and is quite flat over its 10 km extent - features characteristic of bright spots in sedimentary strata. Bright spots in sedimentary strata commonly result from interfaces between fluids of differing densities or between a gas and a fluid, trapped within porous sedimentary rock. At mid-crustal depth most gases only exist in a supercritical phase. Preliminary calculations indicate that the Surrency bright spot has a reflection coefficient of .18 to .36, which is extremely high for such deep reflections. It is questionable whether a rock-rock interface at this depth could produce such a reflection coefficient. The bright reflection occurs within a broad zone of complex dipping reflections that extend downward through the crust, and which have been suggested to mark a Paleozoic suture zone. The authors speculate that the Surrency bright spot may represent formation and/or metamorphic fluids trapped within underthrust sedimentary strata.
Research Organization:
Cornell Univ., Ithaca, NY (USA)
OSTI ID:
5951893
Report Number(s):
CONF-8510489-
Conference Information:
Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 36
Country of Publication:
United States
Language:
English