Clay mineral reactions in clastic diagenesis
Conference
·
· Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:6326232
Studies of clastic sediments have documented the formation and transformation of clay mineral assemblages during burial diagensis. The transformation of smectite to illite in shale by its reaction with the decomposition products of detrital K-feldspar and mica results in the production of new pore water at depth. The overall reaction mobilizes all the major chemical components in the shale, most of which are consumed in the formation of the diagenetic assemblage illite/smectite + chlorite + quartz. However, part of all the components is undoubtedly transported from the shale to sandstone units and is involved in cementation, replacement, and diagenetic clay mineral formation in these reservoir rocks. In contrast to burial diagenetic reactions in shale, where the sequence is monotonic and reasonably predictable, diagenetic reactions in sandstone are frequently variable. This variability is probably attributable to the fact that sandstones are open systems in which the reactions that proceed are controlled in part by the influx of new pore water, the chemistry of which is determined by an outside source. The useful understanding role of clay minerals in hydrocarbon exploration will follow from a determination of the system shale/sandstone/organic material. We need to tie in the nature and timing of shale mineral reactions and their control on the fluid and mass transfer from shale to sandstone.
- Research Organization:
- Univ. of Illinois, Urbana
- OSTI ID:
- 6326232
- Report Number(s):
- CONF-8304200-
- Conference Information:
- Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 67:3
- Country of Publication:
- United States
- Language:
- English
Similar Records
Diagenesis of upper Cretaceous Teapot sandstones, Powder River basin, Wyoming
Effects of provenance on clay diagenesis and porosity in upper Wilcox Formation
Clay-mineral transformation as an indicator of depositional and diagenetic conditions in Pennsylvanian black shales, Paradox Member of the Hermosa Foundation, Utah and Colorado
Conference
·
Sat Mar 31 23:00:00 EST 1984
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:6641957
Effects of provenance on clay diagenesis and porosity in upper Wilcox Formation
Conference
·
Tue Feb 28 23:00:00 EST 1989
· AAPG Bull.; (United States)
·
OSTI ID:5798925
Clay-mineral transformation as an indicator of depositional and diagenetic conditions in Pennsylvanian black shales, Paradox Member of the Hermosa Foundation, Utah and Colorado
Conference
·
Sun Aug 01 00:00:00 EDT 1993
· AAPG Bulletin (American Association of Petroleum Geologists); (United States)
·
OSTI ID:6699875
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
CLAYS
DEPOSITION
DIAGENESIS
EXPLORATION
GEOLOGIC DEPOSITS
GEOLOGIC HISTORY
MINERAL RESOURCES
NATURAL GAS DEPOSITS
PETROLEUM DEPOSITS
RESOURCES
ROCKS
SEDIMENTARY ROCKS
SEDIMENTS
SHALES
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
CLAYS
DEPOSITION
DIAGENESIS
EXPLORATION
GEOLOGIC DEPOSITS
GEOLOGIC HISTORY
MINERAL RESOURCES
NATURAL GAS DEPOSITS
PETROLEUM DEPOSITS
RESOURCES
ROCKS
SEDIMENTARY ROCKS
SEDIMENTS
SHALES