At passive continental margins, such as that offshore of Angola, a dÃ©collement of this mineral cancreate rafts, or fault blocks separated by extreme extension. Contraction of two stratal units separated bythis mineral can result in the formation of a teardrop-shaped deposit of this mineral and the creation ofnamesake weld where the stratal units meet. Processes that lead to the formation of intrusions of thismineral can be classified as active, reactive and passive, in which it takes place by downbuilding. TheZagros Mountains in Iran are known for their glaciers of this mineral. Because deposits of this mineral aremostly nonporous, their density does not increase when they are buried. Due t
At passive continental margins, such as that offshore of Angola, a dÃ©collement of this mineral cancreate rafts, or fault blocks separated by extreme extension. Contraction of two stratal units separated bythis mineral can result in the formation of a teardrop-shaped deposit of this mineral and the creation ofnamesake weld where the stratal units meet. Processes that lead to the formation of intrusions of thismineral can be classified as active, reactive and passive, in which it takes place by downbuilding. TheZagros Mountains in Iran are known for their glaciers of this mineral. Because deposits of this mineral aremostly nonporous, their density does not increase when they are buried. Due to that, deposits of thismineral become less dense than the overburden and can flow upwards to form diapirs, such as domes, andcreate stratigraphic traps where hydrocarbons can be found. Flats of this mineral are commonly left behindin arid regions where the rate of precipitation is exceeded by the rate of evaporation. For 10 points, identifythis mineral whose movement is studied in halokinesis and is the mineral form of sodium chloride.
At passive continental margins, such as that offshore of Angola, a dÃ©collement of this mineral cancreate rafts, or fault blocks separated by extreme extension.
rock salt [or halite]