by Gelogia Team | Feb 12, 2025 | Petrology
Intergrowth texture forms when two minerals crystallize together or through exsolution in igneous rocks. Common types include graphic, myrmekite, exsolution, cavity, radiate, reaction, and pegmatite textures, each revealing mineral interactions and cooling history....
by Gelogia Team | Feb 10, 2025 | Petrology
Types of Metamorphic Texture form due to varying pressure and temperature conditions. They are classified into foliated (slaty, schistose, phyllitic, gneissic) and non-foliated (granulose, mylonitic, hornfelsic) textures. Other textures like augen, porphyroblastic,...
by Gelogia Team | Feb 1, 2025 | Petrology
Types of Protoliths: The following rock properties allow the recognition of protoliths: Relict fabrics: In low-grade metamorphic rocks where recrystallization has not created large new grains or substantial deformation has not taken place, boundaries of original...
by Gelogia | Jan 26, 2025 | Petrology
Deviatoric Stress or Directed Pressure: Deviatoric stress is produced by tectonic forces in the Earth, such as plate motions; this pressure brings about change to produce foliations and lineation’s. This is commonly represented in terms of three stress values in the...
by Gelogia Team | Jan 24, 2025 | Petrology
Sedimentology, the study of sedimentary rocks and their formation, is essential in geology. Its applications span engineering, petroleum, hydrogeology, economic geology, environmental science, and paleontology. What is Sedimentology? There is a term called...
by Gelogia | Jan 8, 2025 | Petrology
Regional metamorphism actively transforms rocks over substantial regions under the influence of excessive temperature and pressure. Unlike contact metamorphism, which occurs in localized zones, It accompanies large-scale tectonic activities, such as mountain-building...