CORSICA BUKU YANG BERKAIT DENGAN «ANTICLINORIA»
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ANTICLINORIA AND SYNCLINORIA. The cross section of the Chinghiz range
under consideration is composed of four synclinoria divided by three anticlinoria (
fig. 3, left). As it was noted earlier anticlinoria represent the exposure of the lower
...
2
The Earth's Crust and Upper Mantle: Structure, Dynamic ...
We can distinguish anticlinoria as structural uplifts and syn- clinoria as structural
depressions. Both of them are hundreds of kilometers long and tens of kilometers
wide. It is quite natural that ancient deposits, some of which have originated ...
3
Vertical Coupling and Decoupling in the Lithosphere
Large anticlinoria. and inferred thrust or reverse faults, occur on the southwestern
side of the Palos Verdes fault zone for a distance of 60-75 km along strike, from
San Pedro Bay to Santa Monica Bay (Nardin & Henyey 1978). These structures ...
4
Geology of the Curlew Quadrangle, Ferry County, Washington
The synclinorium rises to the northeast and disappears as the Evitts Mountain
and Tussey Mountain anticlinoria coalesce about 3 miles northeast of the
mapped area near Beans Cove in Pennsylvania. It disappears to the southwest
as the ...
Raymond Laurence Parker, James Alfred Calkins, 1964
5
U.S. Geological Survey Professional Paper
Thus the Moeda syncline formed between two large anticlinoria, one to the east
and one to the west. Most of the root structures of the anticlinoria have been
obscured by granitization of the sedimentary rocks or by the intrusion of great
masses ...
6
Precambrian Geology of the USSR
The terrain contains two zones, according to the assemblages in the main
geosynclinal complex: an external miogeosynclinal zone in the west and an
internal eugeosynclinal zone in the east, in which there are anticlinoria and
synclinoria.
D.V. Rundqvist, F.P. Mitrofanov, 1993
7
Geological Survey Professional Paper
The Green Mountains and Berkshire Hills are anticlinoria, the first with a steep
west flank, the second overthrust westward. The Hudson Highlands and Reading
Prong have commonly been interpreted as fault-bounded horsts, but modern
work ...
Geological Survey (U.S.), 1976
8
Basic Problems in Geotectonics
Third, the continuous folds in the flanks of anticlinoria usually show a regular
inclination: they are inclined and overturned in both flanks toward the adjacent
depressions, and as a whole they resemble a fan (Fig. 67). If an anticlinorium is ...
Vladimir Vladimirovich Belousov, 1962
It is because of this limited reach of the deforming stress that anticlinoria which by
construction imply the simultaneous development of similar and approximately
equal anticlines throughout the length of a flatly extended arch of strata3 are ...
Thomas Chrowder Chamberlin, 1914
10
Structural Concepts and Techniques I: Basic Concepts, ...
However, the encountering of similar faults at depth under several other major
anticlinoria indicates that perhaps all of the major anticlinoria overlie such faults.
Furthermore, the enveloping surface (connecting the same stratigraphic unit on
the ...
Norman H. Foster, Edward A. Beaumont, American Association of Petroleum Geologists, 1988
