The origin and geologic evolution of the East Continent Rift Basin
Conference
·
· Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5578921
- Univ. of Kentucky, Lexington, KY (United States). Kentucky Geological Survey
The East Continent Rift Basin (ECRB) is a newly recognized, dominantly sedimentary-volcanic Proterozoic rift basin that apparently represents the southern extension of the Keweenawan Midcontinent Rift. The ECRB extends from central Michigan at least as far south as south-central Kentucky. The inferred age of the rift fill is approximately 1,000 Ma. Evidence supporting a rift origin for the ECRB includes: interbedding of continental flood basalts and felsic volcanics with siliciclastics; sedimentary fill consisting of distal, arid-climate alluvial fan sediments that lack metamorphic lithologies; close proximity and similar lithologic succession to the Keweenawan rift-fill rocks of the Michigan Basin; and inferred marginal block faulting of Granite-Rhyolite Province rocks near the western edge of the ECRB. ECRB evolution is interpreted as follows: (1) formation of Granite-Rhyolite Province rocks (1,500--1,340 Ma); (2) Keweenawan crustal extension and rifting with development of central mafic complexes, emplacement of volcanic rocks, and deposition of siliciclastic fill from eroded marginal Granite-Rhyolite Province tilted fault blocks (ca 1,000 Ma); (3) overthrusting of the Grenville allochthon and associated foreland thrusting and folding of the rift sequence rocks together with deposition of foreland basin sediments (975---890 Ma); (4) Late Proterozoic erosional removal of the foreland basin sediments and interpreted wrench faulting along the Grenville Front (post-975 to pre-570 Ma); and (5) tectonic inversion, with the ECRB area remaining relatively high during major cambrian subsidence in central Kentucky (590--510 Ma).
- OSTI ID:
- 5578921
- Report Number(s):
- CONF-921058--
- Conference Information:
- Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 24:7
- Country of Publication:
- United States
- Language:
- English
Similar Records
Stratigraphy, structure, and extent of the East Continent Rift Basin
The Midcontinent rift system and the Precambrian basement in southern Michigan
Grenville foreland thrust belt hidden beneath the eastern US midcontinent
Conference
·
Tue Dec 31 23:00:00 EST 1991
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5578939
The Midcontinent rift system and the Precambrian basement in southern Michigan
Conference
·
Thu Mar 31 23:00:00 EST 1994
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:7123436
Grenville foreland thrust belt hidden beneath the eastern US midcontinent
Journal Article
·
Thu Dec 31 23:00:00 EST 1992
· Geology; (United States)
·
OSTI ID:6043181
Related Subjects
58 GEOSCIENCES
580000* -- Geosciences
AGE ESTIMATION
DEVELOPED COUNTRIES
GEOLOGIC AGES
GEOLOGIC HISTORY
GEOLOGIC MODELS
GEOLOGIC STRUCTURES
GEOLOGY
IGNEOUS ROCKS
KENTUCKY
LITHOLOGY
MICHIGAN
NORTH AMERICA
OHIO
ORIGIN
PETROLOGY
PRECAMBRIAN ERA
RIFT ZONES
ROCKS
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
USA
VOLCANIC ROCKS
580000* -- Geosciences
AGE ESTIMATION
DEVELOPED COUNTRIES
GEOLOGIC AGES
GEOLOGIC HISTORY
GEOLOGIC MODELS
GEOLOGIC STRUCTURES
GEOLOGY
IGNEOUS ROCKS
KENTUCKY
LITHOLOGY
MICHIGAN
NORTH AMERICA
OHIO
ORIGIN
PETROLOGY
PRECAMBRIAN ERA
RIFT ZONES
ROCKS
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
USA
VOLCANIC ROCKS