nappe การใช้

The Br関enne Unit is an ophiolitic nappe of Upper Devonian age.
The klippe is the isolated block of the nappe overlying autochthonous material.
Nappe flow regimes occur for small discharges and flat slopes.
The Ponga Nappe Province is to the east of the Central Coal Basin,
Special subduction related metamorphism to blueschist facies is known from the B魊ka nappe.
The term nappe is used for the sheet of water flowing over the weir.
Cho Nappe is considered as rootless nappe.
Cho Nappe is considered as rootless nappe.
The Slatnik Formation can be found in the Kobla Nappe and the Tolmin Nappe.
The Slatnik Formation can be found in the Kobla Nappe and the Tolmin Nappe.
Nappe flow has pockets of air at each step whereas skimming flow does not.
The Alps north of the Periadriatic Seam are usually divided into three large nappe complexes.
Internally, the rocks of the nappe are isoclinally folded and cut by shear zones.
The flow over a stepped spillway is classified as either nappe flow or skimming flow.
This formed the Betic nappe stack.
These data allowed Kamaletdinov to create a global geological theory that he called nappe-thrust.
He was a proponent of the nappe concept and of tectonics as a mountain-building force.
Kr?~ Ha Nappe is dominantly composed of rock, that were formed in the Zliechov basin.
In particular, an ellipse has two Dandelin spheres, both touching the same nappe of the cone.
The nappe is named after the mountain Dent Blanche, which is formed by rocks of the nappe.