fault block वाक्य
उदाहरण वाक्य
मोबाइल
- The dismemberment and subsidence of continental crust into horsts, rotated fault blocks and half-grabens that underlie the Spratly Islands and surrounding sea bottom occurred in 2 distinct periods.
- The missing part of the Dox Formation and overlying Cardenas Basalt and Chuar Group can be found in a prominent syncline and fault block in the eastern Grand Canyon.
- Oriented generally north to south, the Trout Creek Mountains consist primarily of fault blocks of basalt, which came from an ancient volcano and other vents, on top of older metamorphic rocks.
- Mount Tymfi represents a series of uplifted fault blocks and faulted escarpments and is largely composed of Palaeocene-Eocene limestone, with some exposures of Campanian-Jurassic dolomite and limestone on the northern scarp.
- Genel took the opportunity because of encouraging indications including onshore oil seeps and existing geological data showing favourable conditions for hydrocarbons to have accumulated in numerous large tilted fault blocks and sub-basins.
- Because the fault block is uplifted on one side along the Eger trough and the border diverges away from the ridge line, the Ore Mountains reach their greatest height on the Bohemian side.
- Climbing from the Tularosa Basin of the later Trinity Test Site and White Sands Missile Range into the Sacramento Mountain fault block escarpments required numerous trestles, switchbacks and grades as steep as 6.4 percent.
- Most seismicity within the Gran Desierto originates at depths of five to six kilometers, corresponding to the transition between uplift is still occurring along the Mesa Arenosa, a drag folded fault block forming the coastal boundary.
- When the region was broken into fault blocks and the blocks were uplifted and tilted, the back slope of each block was a part of the previously eroded surface and the face of the block was a surface of fracture.
- The Visund fault block and the Oseberg-Brage infill are examples from marine half-grabens which are near the central or axial zones of the northern North Sea rift complex, far from the main hinterland areas and show deepening upward trends into basinal shales.
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