• खंडज डाइक | |
clastic: खंडज खंडनीय | |
dike: नहर नाला नाली बंद | |
clastic dike मीनिंग इन हिंदी
clastic dike उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- Clastic dikes are formed when sediment fills a pre-existing crack.
- Clastic dikes are commonly vertical or near-vertical.
- Clastic dikes are found in sedimentary basin deposits worldwide.
- Formal geologic reports of clastic dikes began to emerge in the early 19th century.
- A "'clastic dike "'is a seam of sedimentary material that fills an open strata or layering in other rock types.
- Clastic dikes form rapidly by fluidized injection ( mobilization of pressurized pore fluids ) or passively by water, wind, and gravity ( sediment swept into open cracks ).
- The age of these deposits is demonstrated by the presence of multiple interglacial calcretes interbedded in these glaciofluvial deposits, sequences of sediments with normal, reverse, and normal magnetostratigraphy, optically stimulated luminescence dating, and unconformity truncated clastic dikes.
- Based on the presence of multiple interglacial calcretes interbedded with flood deposits, magnetostratigraphy, optically stimulated luminescence dating, and unconformity truncated clastic dikes, it has been estimated that the oldest of the Pleistocene Missoula floods happened before 1.5 million years ago.
- Based on the presence of multiple interglacial calcretes interbedded with glaciofluvial flood deposits, magnetostratigraphy, optically stimulated luminescence dating, and unconformity truncated clastic dikes, it has been estimated that the oldest of these megafloods flowed through the Channel Scablands sometime before 1.5 million years ago.
- :Results from analytical modeling of clastic dike injection in soft rocks indicate propagation occurred at a rate of approximately 4 to 65 m / s at driving pressures of 1-2 MPa . Emplacement duration ( < 2 s ) is similar to the speed with which acoustic energy ( pressure waves ) moves through partially lithified sedimentary rock.