Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Clay minerals as indicators for depositional environment in the south Hallettsville Field, Lavaca County, Texas

Conference · · Trans., Gulf Coast Assoc. Geol. Soc.; (United States)
OSTI ID:6372974
The South Hallettsville Field, Lavaca County, Texas, produces gas and condensate from Lower Wilcox sandstones and shales which have been interpreted as either channel turbidite deposits in outer-shelf to slope locations or as delta to pro-delta sands and muds. Thirteen core samples were analyzed by X-ray diffraction methods to determine whether a semiquantitative estimate of clay mineral content would aid in determining the depositional environment. Discrete illite, kaolinite, and chlorite are of particular interest because the presence of these minerals is interpreted as being due to original deposition. If a turbidity-type event occurred, the weight percents of nondiagenetic clays in this sequence should: (1) decrease significantly as the boundary is crossed between the shale and the overlying sandstone; and (2) gradually increase in progressively shallower samples within the sandstone. However, the weight percents for kaolinite and chlorite do not vary significantly; the illite content gradually decreases with shallower depths. This sequence is more compatible with a deltaic environment of deposition. 10 references.
OSTI ID:
6372974
Conference Information:
Journal Name: Trans., Gulf Coast Assoc. Geol. Soc.; (United States) Journal Volume: 30
Country of Publication:
United States
Language:
English