Role of H2O and CO2 in Silicate melt
H2O and CO2 are the two most important components of fluids in the upper mantle and crust, and their solubilities […]
Role of H2O and CO2 in Silicate melt Read More »
H2O and CO2 are the two most important components of fluids in the upper mantle and crust, and their solubilities […]
Role of H2O and CO2 in Silicate melt Read More »
On the basis of mineral replacement and intergrowths, four oxide series are recognized among the sandstones – Stages of diagenesis
Stages of Diagenesis of Sandstone Read More »
Rules of substitution Terminology related to partitioned between the solid & liquid phase Distribution coefficients and Geothermometers Distribution coefficient (D)
Ionic Substitution in Minerals/ Crystals Read More »
Fick’s Law of Diffusion in Igneous Petrology Fick’s law describes the movement of elements and ions due to concentration gradients,
Fick, Roult and Henry’s law in petrogenesis Read More »
Three major cycles of deposition have been found in the sedimentary records of the Mesozoic formations of the Spiti Basin.
Magnetostratigraphy is based on the polarity of the earth’s magnetic field as it is preserved in the sediments at the
Magnetostratigraphy Read More »
Biostratigraphy deals with the classification and correlation of rock strata based on their fossil contents. Fossils help in assigning relative
The Continuous Paleozoic succession is beautifully exposed in the area of Spiti valley. A rich collection of fossils reported from
Paleozoic of Spiti Read More »
Any natural phenomena that obey a definite law of flow rate can be used to mark off certain intervals of
Chronostratigraphy Read More »
We can classify the layered rock sequences primarily on the basis of their lithological characters. This scheme of classification is