GEO-ARTICLES

Red Field Ratio

The Redfield ratio is the consistent atomic ratio of carbon, nitrogen and phosphorous found in marine phytoplankton and throughout the deep oceans (C:N:P = 106:16:1). When nutrients are not limiting, the molar elemental ratio C:N:P in most phytoplankton is 106:16:1 In the ocean, a large portion of the biomass is found to be nitrogen-rich plankton. Many of these plankton

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Exploring the Marvels of Geological Time: Unveiling Earth’s Epochs

The study of geology offers a captivating journey through time, unveiling the intricate tapestry of Earth’s history. Spanning billions of years, this narrative is composed of distinct epochs, each characterized by unique geological events and transformations. In this article, we delve into the fascinating world of geological time, exploring the epochs that have shaped our

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Anorthosites

Anorthosites are defined as plutonic rocks with over 90% plagioclase. They are highly felsic, felsic minerals, however is a Calcic plagioclase, which along with subordinate associated high temperature mafic minerals. The anorthosites can be classified as Archaean and Proterozoic – Archaean Anorthosites :- Most Archaean anorthosites cluster in the range 3.2 to 2.8 Ga. They

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Chromium (Cr) Deposits

Important minerals : Types of chromite deposits :- Indian deposits :- Stratiform or Layered Chromite Associated with mafic/ ultramafic layered intrusions formed in calm environment (Precambrian) Podiform chromite Irregular geometry, found in disturbed environment, Phanerozoic in age Sukinda ultramafic complex, Orissa Stratified beds inclosed in a sequence of Dunite-peridotite Sithampundi chromite, Tamilnadu Stratiform deposit in

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