synclinal वाक्य
उदाहरण वाक्य
मोबाइल
- The Anthracite Valley Section is a crescent-shaped synclinal basin.
- The western half of the basin occupies a trough of synclinal structure.
- There is a large amount of anticlinals, synclinals, diaclases, faults.
- Geologically, House Mountain is a " synclinal outlier " of Clinch Mountain.
- A strong synclinal fold traverses Eday and Shapinsay, the axis trending north-south.
- In the synclinal of the Bogot?savanna, the thickness of Guaduas varies between and.
- McCauley Mountain is a synclinal mountain.
- Synclinal deflection below the origin ( dotted line ) is shown marked by the A3 and A4.
- IUPAC defines groups as gauche if they have a " synclinal alignment of groups attached to adjacent atoms ".
- The mountain also has an elbow which is part of a double synclinal that heads eastward to Nescopeck Mountain.
- The high walls of Wilpena Pound are formed by the outcropping beds of the eponymous Pound Quartzite in a synclinal structure.
- The Ely synclinal fold, produced 70 million metric tons from the Chandler, Pioneer, Zenith, Sibley and Savoy mines.
- Crystal Grottoes is an example of a solutional cave, formed in a karst environment within a synclinal occurrence of Tomstown Dolomite.
- Two ways to maintain volume conservation are thickening of units and synclinal deflection of incompetent material; it is likely that both may occur.
- Geologically, the Gulf is the result of the Arab Gulf Synclinal Basin, one of a succession of synclines along the northern coast of Africa.
- The Vindhyas do not form a single range in the proper geological sense : the hills collectively known as the Vindhyas do not lie along an synclinal ridge.
- The anthracite fields are maintained in synclinal basins that are surrounded by sandstone ridges, which help to protect the anthracite ( Hornberger et al ., 20-2 ).
- Overall, this region reveals the interior of this thrusted anticlinal-synclinal structure and presents a phenomenal exposure of complex central Appalachian macroscale structures involving the Silurian-Devonian package of rocks.
- Continued shortening and excess material within the anticlinal core not only results in increased amplitude and disharmonic folds, but may lead to the onset of thrusts out of the folded synclinal or anticlinal regions.
- Thrust faults in the synclinal fold, if any formed, may also be rotated to assist in the formation of detached lift-off folds upon further tightening and rotation ( figure 4 ).
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