| • क्रमिक संस्तर • क्रमिक संस्तरण | |
| graded: अनुस्तरित प्रवणित | |
| bedding: बिस्तर शय्या | |
graded bedding मीनिंग इन हिंदी
graded bedding उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- These occur in thin beds exhibiting graded bedding reminiscent of placer sorting.
- Although graded bedding can form in many different environments, it is a characteristic of turbidity currents.
- In low-strain zones they preserve graded bedding, cross-bedding and heavy mineral-rich horizons.
- Graded bedding is a structure where beds with a smaller grain size occur on top of beds with larger grains.
- Classic, low-density turbidites are characterized by graded bedding, bedding, and an absence of shallow-water features ( Fairbridge, 1966 ).
- This resulted in layers with graded bedding, or bedding in which the larger particles are at the bottom and the smaller ones are at the top.
- Sedimentary structures such as cross bedding, graded bedding and ripple marks are utilized in strata in geologically complex terrains and understand the depositional environment of the sediment.
- The folded or deformed, recognising younging indicators or graded bedding is critical to interpretation of the sedimentary section and often the deformation and metamorphic structure of the region.
- They include ripple marks; mudcracked surfaces; cone-in-cone structures; interformational breccias / conglomerates; both normal and reversed small-scale, graded bedding; and local channel fills.
- In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e . g ., tabular and trough cross-bedding and graded bedding.
