1 edition of Geology of the Alabama inner piedmont terrane found in the catalog.
Geology of the Alabama inner piedmont terrane
by Geological Survey of Alabama, Mineral Resources Division in Tuscaloosa, Ala
Written in English
|Statement||by Mark G. Steltenpohl ... [et al.].|
|Series||Bulletin / Geological Survey of Alabama ;, 139, Bulletin (Geological Survey of Alabama) ;, 139.|
|Contributions||Steltenpohl, Mark G.|
|LC Classifications||QE81 .A15 no. 139|
|The Physical Object|
|Pagination||76 p. :|
|Number of Pages||76|
|LC Control Number||90621824|
Thomas E. West, Structural analysis of the Carolina‐Inner Piedmont terrane boundary: Implications for the age and kinematics of the central Piedmont suture, a terrane boundary that records Paleozoic Laurentia‐Gondwana interactions, Tectonics, /98TC, 17, 3, (), (). Bentley, R.D. and T.L. Neathery, , ‘Geology of the Brevard fault zone and related rocks of the Inner Piedmont of Alabama.’ Alabama Geological Society Field Trip Guidebook, p. Google Scholar.
Get this from a library! Geology of the Brevard fault zone and related rocks of the inner Piedmont of Alabama. [Robert Donald Bentley; Thornton Lee Neathery; Alabama Geological Society.]. Research Interests. Field and laboratory research on structural geology and tectonics, metamorphic and igneous rocks, impact craters and related materials, fault zones and fault rocks, mountain chains, Appalachian Piedmont and Blue Ridge geology, pre-Cretaceous terranes and buried basins beneath the Atlantic and Gulf coastal plains, intraplate earthquakes, and hydrogeology of fractured.
___, R. B. Cook, and D. E. Brown, , Tectonic evolution of the western part of the Pine Mountain window and adjacent Inner Piedmont province; pp. 1–13 in J. W. Sears (ed.), Contrasts in Tectonic Style Between the Inner Piedmont Terrane and the Pine Mountain Window: Alabama Geological Society, 18th Annual Field Trip Guidebook, 61 p. Inner Piedmont Pine Mountain window Carolina & Uchee terranes Coastal Plain T w alig a Coastal Plain onlap Coastal Plain exotic volcanic rocks Caro lina terrane fault M odoc f. galoo terrane terrane GA SC FL AL TN NC Gondwana (African-affinity) rocks 15 14 13 11 12 10 Fig. 1B Figure 1 (continued on following page). (A) Map of the major orogenic.
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The Inner Piedmont is a large, composite, sillimanite-grade terrane that extends from near the Virginia–North Carolina border to central Alabama and consists of the eastern Tugaloo and Cat Square terranes. It is bound to the west by the Brevard fault zone and to the east by the central Piedmont suture.
interpretation for mid-crustal level channelized flow of the Inner Piedmont terrane. The Opelika Complex is not related to the Inner Piedmont, as is traditionally thought, but is continuous with the eastern Blue Ridge around the hinge zone of the Tallassee synform as originally suggested by Grimes et al.
(a). Abstract. The Inner Piedmont extends from North Carolina to Alabama and comprises the Neoacadian (– Ma) orogenic core of the southern Appalachian orogen.
Bordered to west by the Blue Ridge and the exotic Carolina superterrane to the east, the Inner Piedmont is cored by an extensive region of migmatitic, sillimanite-grade rocks. Inner Piedmont is divided into two groups of rocks, Dadeville and Opelika Complexes (Bentley and Neathery, ), divided by Stonewall line.
Dadeville Complex consists of Agricola Schist, Waresville Schist, Camp Hill Gneiss, Chattasofka Creek Gneiss, Ropes Creek Amphibolite, Waverly Gneiss, Simmons Crossroads metagranite (informal), and various unnamed mafic and ultramafic intrusive.
Bentley, R.D. (editor), and Neathery, T.L. (editor),Geology of the Brevard fault zone and related rocks of the Inner Piedmont of Alabama: Alabama Geological Society Annual Field Trip Guidebook, December, no.
8, p. The Inner Piedmont is bounded on the northwest and southeast by narrow, intensely folded, highly sheared, and partially cataclastic belts of lower-grade rocks. The northwest belt is termed the Non-migmatitic-Brevard belt; the southeast belt is herein called the Kings Mountain-Wacoochee belt.
Through STATEMAP, The Geological Survey of Alabama has completed and published more than 50 new geologic maps at the minute (,) scale, and several more are in progress. The maps are color plots and are accompanied by explanations and booklets summarizing the geology. Alabama Rocks Alabama's diverse geology has produced great variation in terrain and physiography, ranging from the coastal lowlands of the southern part of the state to rugged mountainous areas of the north.
Physiographically, the state is divided into five sections: the Cumberland Plateau, Highland Rim, Valley and Ridge, Piedmont Upland, and East Gulf Coastal Plain. Callan Bentley teaches geology at Piedmont Virginia Community College in Charlottesville, Virginia.
He is a Fellow of the Geological Society of America. For his work on this blog, the National Association of Geoscience Teachers recognized him with the James Shea Award.
The Piedmont is a plateau region located in the Eastern United sits between the Atlantic coastal plain and the main Appalachian Mountains, stretching from New York in the north to central Alabama in the south. The Piedmont Province is a physiographic province of the larger Appalachian division which consists of the Gettysburg-Newark Lowlands, the Piedmont Upland and the Piedmont.
The Inner Piedmont is composed of the Waresville Schist, a diverse group of metamorphosed volcanic and volcaniclastic rocks that has been intruded by the Rock Mills Granite Gneiss. boundary between the Inner Piedmont and the Charlotte terrane. A total of eleven and possibly twelve westward transported crystalline thrust sheets compose these ter ranes in the Greenville quadrangle.
The Blue Ridge terrane consists of a stack of five thrust sheets; the Inner Piedmont is underlain by four and possibly five thrust sheets, and. Geology and ground water of the Piedmont area of Alabama, Files: Type: Chambers County.
Number Title CC: Hydrogeology and vulnerability to contamination of major aquifers in Alabama: Area 5, Geology of the Alabama Inner Piedmont Terrane, Files: Type: CC: Hydrogeology and vulnerability to contamination of major.
The southern Appalachian Inner Piedmont consists of the Tugaloo and Cat Square terranes, which are separated by the Brindle Creek fault (Bream et al., (Bream et al., Bream, Bream. Get this from a library. Contrasts in tectonic style between the inner Piedmont terrane and the Pine Mountain window in eastern Alabama and adjacent Georgia.
[James W Sears; Alabama. Steltenpohl, M. G., et al. "Geology of the Alabama Inner Piedmont Terrane." Geological Survey of Alabama Bulletin Tuscaloosa: Geological Society of Alabama, Yokal, L. S., et al. "Comparison of the Pine Mountain Block Basement-Cover Sequence with the Lower Cambrian Clastic-Carbonate Sequence of the Talladega Slate Belt.".
a digital regional geologic map of the northern alabama piedmont constructed with gis. David T. Allison, Dept. of Earth Sciences, University of South Alabama, Mobile, AL Recent knowledge gained from a program of converting mapping data to digital geologic maps has demonstrated that GIS is superior to traditional methods of producing.
Alabama; Pleistocene vertebrate assemblage Little Bear Cave, Colbert Co., Alabama; $ 17b Geology of the Pine Mountain window and adjacent terranes in the Piedmont Province of Alabama and Georgia, SE Section Geological Society of America, Mar.
$ 18 Contrasts in tectonic style between the Inner Piedmont terrane and the. New field mapping along the Carolina‐Inner Piedmont terrane boundary in South Carolina and eastern Georgia reveals preaccretionary, synaccretionary, and postaccretionary faults.
The dextral strike‐slip Lowndesville shear zone is adjacent to a ∼50‐km‐long segment of the terrane boundary. To promote geology as a profession and as a science; On November 1,the Society was incorporated with the Articles of Incorporation entered in B pages at the Tuscaloosa County Probate Office.
Orogen-parallel transport of the Piedmont in east Alabama NovemberAlexander City, Alabama. "The Appalachians constitute one of Earth's major tectonic features and have served as a springboard for innovative geologic thought for more than years.
This volume contains 36 original papers reporting the results of research performed throughout nearly the entire length and breadth of the Appalachian region, including all major provinces and geographical areas.It is proposed that the SSR amphibole cores were metamorphosed probably during terrane–terrane collision under amphibolite facies conditions, with the actinolite rims possibly being formed during thrusting of the SSR rocks onto the continental margin.
and Whitney, J.A. Geology of the Inner Piedmont, Carolina Terrane, and Modoc Zone. The Inner Piedmont (IP) consists of a middle to upper amphibolite facies assemblage of para- and orthogneisses that extends from northern North Carolina to the Coastal Plain in Alabama wherein the dominant foliation has a characteristic gentle dip (Fig.
1, Fig. 2).