একটি গম্বুজ শিলা গঠন যেখানে শিলা একটি মূল উর্ধ্বগামী সরানো এবং আরও ভঙ্গুর উপরিতলের স্তরে এনেছে করেছে

diapirs's Usage Examples:

Depending on the tectonic environment, diapirs can range from idealized mushroom-shaped Rayleigh–Taylor-instability-type.

of relatively buoyant magma in large masses called plutonic diapirs.

Because the diapirs are liquified and very hot, they tend to rise through the surrounding.

Kerguelen hotspot was split into several diapirs of various sizes, composition, and ascent rates.

These separate diapirs created the Bunbury Basalt, the Southern.

dome-shaped forms called diapirs when doing so.

On Earth, salt domes are salt diapirs in the crust which rise through surrounding rock.

At a late stage, diapirs tend to initiate at the junctions between ridges, their growth fed by movement.

The extremely hot, relatively buoyant plutons, also called plutonic diapirs, intruded through denser, native country rock and sediments, never reaching.

Mud, rich in organic molecules intrudes all of these units with diapirs—rising tendrils of mud with behavior similar to salt domes.

caused the underlying shale Akata Formation to be squeezed into shale diapirs.

Separation of metal from rock in a primordial magma ocean; 3) Migration of iron diapirs or dikes through the mantle.

can generate large salt structures such as underground salt layers, salt diapirs or salt sheets at the surface.

Most exposures of this sequence are in the form of emergent salt diapirs within anticlines of the Zagros fold and thrust belt.

crust in pull-aparts may generate differential loading and instigate salt diapirs to rise, a frequent trap for hydrocarbons.

One suggests that hotspots are due to mantle plumes that rise as thermal diapirs from the core–mantle boundary.

mantle, overlain by massive gabbro, with dunite bodies left from mantle diapirs.

is granitic, having been formed 210 to 80 million years ago as igneous diapirs 6 miles (10 km) below the surface.

extensions of salt tectonics that form at the Earth's surface when either diapirs or salt sheets pierce through the overlying strata.

basin owes its shape to ongoing salt tectonics and is surrounded by salt diapirs.

debate concerning the nature and origin of the Mt Desire Dyke and other 'diapirs' of the Flinders Ranges, including: typical dolomitic breccia and a large.

These are reactive diapirs, active diapirs, and passive diapirs.

Reactive diapirs initiate and grow beneath grabens from normal.

diapirs's Meaning':

a domed rock formation where a core of rock has moved upward and pierced through the more brittle overlying strata

Synonyms:

formation; geological formation;

Antonyms:

natural depression; natural elevation; finish;