Tools

LEADER 03532ctm a2200505 i 4500

001 ocm41655250;

003 OCoLC;

005 20240430153657.0;

008 990706s1998 xx ab bm 000 0 eng d;

035 a| (Sirsi) o41655250;

035 a| (OCoLC)41655250;

043 a| n-us-sc;

049 a| EREE;

050 4 a| QE162.C44b| D63 1998;

100 1 a| Doar, William R.,c| III,e| author.=| ^A1405269;

245 10 a| Geology, structure and metamorphic zonation of the Chappells 7.5' Quadrangle, South Carolina /c| by William Richardson Doar, III.;

264 0 c| 1998.;

300 a| v, 50 leaves :b| illustrations (some color), maps ;c| 28 cm;

336 a| textb| txt2| rdacontent;

337 a| unmediatedb| n2| rdamedia;

338 a| volumeb| nc2| rdacarrier;

502 b| M.S.c| East Carolina Universityd| 1998;

500 a| Folded map in pocket in back of book.;

500 a| Submitted to the faculty of the Department of Geology.;

500 a| Advisor: David P. Lawrence;

520 3 a| The Chappells quadrangle. South Carolina, is 35 km west of Columbia and covers the traditional Carolina Slate belt/ Charlotte belt boundary. It contains plutonic, layered metamorphosed sedimentary and volcanic, deformed, and metamorphically altered rocks. These were deposited, intruded, tectonically transported, and some have unknown emplacement histories. The rocks were subjected to several periods of physical deformation (folding, thrusting, shearing, brittle faulting) and metamorphic alteration during the Paleozoic orogenies. The most intense folding deformation is ductile folding in the amphibole and biotite gneisses and the most intense shearing is in the interlayered felsic and mafic volcanic unit. A major structure crossing the center of the quadrangle from west to east dominates the tectonic history with three periods and directions of motion and explains the maximum temperature/pressure gradient of 58.33 °C/ 1 kb per km distance and a bouguer gravity gradient of 2.25 mgal/ km across it. A second structure along the quadrangle's western border may have associated deformations and histories. The most intense metamorphic alteration is in a garnet meta- gabbro with a metamorphic peak granulite grade mineral assemblage of 750 °C/ 10 kb.;

504 a| Includes bibliographical references (leaves 31-34).;

650 0 a| Geologyz| South Carolinaz| Chappells Region.=| ^A1001211;

650 7 a| Geology.2| fast0| (OCoLC)fst00940627;

655 7 a| Academic theses.2| fast0| (OCoLC)fst01726453;

655 7 a| Academic theses.2| lcgft;

655 7 a| Thèses et écrits académiques.2| rvmgf0| (CaQQLa)RVMGF-000001173;

655 2 a| Academic Dissertation.0| (DNLM)D019478?| UNAUTHORIZED;

700 1 a| Lawrence, David P.,d| 1943-e| degree supervisor.=| ^A1461792;

710 2 a| East Carolina University.b| Department of Geology.?| UNAUTHORIZED;

856 41 z| Access via ScholarShipu| http://hdl.handle.net/10342/11952;

949 a| Click on web addressw| asish| joyner101;

949 a| Click on web addressw| asish| hsl111;

994 a| C0b| ERE;

596 a| 1 4;

998 a| 651380;

999 a| ASK AT SPECIAL COLLECTIONS DESKw| ASISc| 1i| 1165983d| 3/25/2002l| JSCJTHDm| JOYNERr| Ys| Yt| JSCJTHDu| 3/25/2002x| ETDz| JSPECCOLLo| .STAFF. 0;

999 a| CLICK ON WEB ADDRESSw| ASISc| 1i| 651380-3001l| JNETm| JOYNERr| Ys| Yt| JNE3ETDu| 4/30/2024x| ETDz| JERESOURCE;

999 a| CLICK ON WEB ADDRESSw| ASISc| 1i| 651380-4001l| HSLELECm| HSLr| Ys| Yt| HEETDu| 4/30/2024x| ETDz| HERESOURCE;

Geology, structure and metamorphic zonation of the Chappells 7.5' Quadrangle, South Carolina / by William Richardson Doar, III.

Author/creator	Doar, William R. author.
Other author	Lawrence, David P., 1943- degree supervisor.
Other author	East Carolina University. Department of Geology.
Format	Theses and dissertations
Production	1998.
Description	v, 50 leaves : illustrations (some color), maps ; 28 cm
Supplemental Content	Access via ScholarShip
Subjects	Geology--South Carolina. --Chappells Region.

Summary	The Chappells quadrangle. South Carolina, is 35 km west of Columbia and covers the traditional Carolina Slate belt/ Charlotte belt boundary. It contains plutonic, layered metamorphosed sedimentary and volcanic, deformed, and metamorphically altered rocks. These were deposited, intruded, tectonically transported, and some have unknown emplacement histories. The rocks were subjected to several periods of physical deformation (folding, thrusting, shearing, brittle faulting) and metamorphic alteration during the Paleozoic orogenies. The most intense folding deformation is ductile folding in the amphibole and biotite gneisses and the most intense shearing is in the interlayered felsic and mafic volcanic unit. A major structure crossing the center of the quadrangle from west to east dominates the tectonic history with three periods and directions of motion and explains the maximum temperature/pressure gradient of 58.33 °C/ 1 kb per km distance and a bouguer gravity gradient of 2.25 mgal/ km across it. A second structure along the quadrangle's western border may have associated deformations and histories. The most intense metamorphic alteration is in a garnet meta- gabbro with a metamorphic peak granulite grade mineral assemblage of 750 °C/ 10 kb.
General note	Folded map in pocket in back of book.
General note	Submitted to the faculty of the Department of Geology.
General note	Advisor: David P. Lawrence
Dissertation note	M.S. East Carolina University 1998
Bibliography note	Includes bibliographical references (leaves 31-34).
Genre/form	Academic theses.
Genre/form	Academic theses.
Genre/form	Thèses et écrits académiques.

Availability

Library	Location	Call Number	Status	Item Actions
Joyner	University Archives	ASK AT SPECIAL COLLECTIONS DESK	✔ Available	Request Material
	Electronic Resources	Access Content Online	✔ Available

Geology, structure and metamorphic zonation of the Chappells 7.5' Quadrangle, South Carolina / by William Richardson Doar, III.

Click here for more information about this title

Availability