On the basis of mineral replacement and intergrowths, four oxide series are recognized among the sandstones – Stages of diagenesis From the type of reaction and the principal sequence of occurence three stages of diagenesis are established as follows – Among sandstones, the progress of diagenesis may be arrested at either the locomorphic or phyllomorphic […]
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Chemical weathering may be defined as the spontaneous and irreversible thermodynamic process that causes degradation of the mineral phases under the prevailing environmental conditions at the surface of the Earth. It is usually considered to be the solid/solution interactive process occurring in contact with the atmosphere. In other words chemical weathering may be defined as that set of processes
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This plot shows the average current velocities necessary for the erosion, transportation and deposition of the sediment particles of different sizes. The lower curve on the diagram, it shows that once eroded and moving a clay particle, but not a fine particles of sand can be transported by a week current. This is because the
HJULSTROM’S DIAGRAM Read More »
Marine isotope stages (MIS), marine oxygen-isotope stages, or oxygen isotope stages (OIS) are alternating warm and cool periods in the Earth’s paleoclimate, deducted from oxygen isotope data derived from deep sea core samples. Working backwards from the present, MIS 1 in the scale, stages with even numbers have high levels of O18 and represents cold
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Sapropel is a term used in marine geology to describe dark-colored sediments that are rich in organic matter. Sapropels events occurs periodically (around each 21000yr) and are specific to the Mediterranean sea. Organic carbon concentration in sapropels commonly exceeds 2% in weight. Their occurrence has been found to be related of the Earth’s orbital parameter.
Sediment can be consist of either mineral or fossil particles, and both types can be found in many places on the bottom of the sea. Classification of marine sedimentation :- The sedimentation can be subdivided on the basis of the size of the particles or on the basis of their mode of formation. Factors that
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