Bundelkhand Craton: Complete Guide to Geology, Structure & Formation | Archean Cratonic Studies

Bundelkhand Craton: Complete Guide to Geology, Structure & Formation | Archean Cratonic Studies

The Bundelkhand Craton is a 26,000 sq. km Archean cratonic block in central India, characterized by a triangular geometry with semi-circular sides. It is named after the 15th-century Bundelkhand kingdom. This geological formation contains tonalite-trondhjemite-granodiorite (TTG) gneisses dating from 3.55–2.5 Ga, Bundelkhand granite complexes, and distinctive supracrustal rock enclaves. The craton is bounded by the Son-Narmada lineament in the south, separated from the Aravalli craton by the Vindhyan basin in the west, and overlain by Indo-Gangetic alluvium in the north.

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d geological map of the Singhbhum Craton, NE India, showing its main lithounits and tectonic margins. Abbreviations: OMG—Older Metamorphic Group. OMTG—Older Metamorphic Tonalite Group. Singhbhum Granite Complex—SBG with SBG-I, SBG-II SBGIII. IOG—Iron Ore Group. UGG—Undifferentiated Granite Gneiss. NSO—Northern Singhbhum Orogen. CGGC—Chotanagpur Granite Gneiss Complex.

The Singhbhum Craton stratigraphy | Singhbhum Craton | location| Map

Introduction of Singhbhum Craton? Singhbhum Craton covers a triangular area of 50,000 sq. km and consists of a core (8,000 sq. km) of Singhbhum granite, rimmed by supracrustals of varied character and age. It covers Jharkhand, Odisha, and adjoining areas in the eastern part of the Indian Shield. Location and Boundaries of Singhbhum Craton The

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Dharwar cratons

The Dharwar Craton: Geological Significance, Structure, and Economic Importance

The Indian shield consists of five major Archean Cratons: Dharwar, Bastar, Singhbhum, Bundelkhand, and Aravalli. The Indian shield, comprising the Precambrian basement, is primarily made up of granitic gneisses and migmatites, known as the Peninsular Gneiss or Fundamental Gneiss. The Peninsular Gneiss was emplaced on an older Greenstone belt, a relic of the Primordial Crust,

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Guide to Chronostratigraphy and the Geological Time Scale: From Chronostratigraphic Units to Modern Dating Techniques

Guide to Chronostratigraphy and the Geological Time Scale: From Chronostratigraphic Units to Modern Dating Techniques

Chronostratigraphy Introduction Lithology (Lithostratigraphy): The stratigraphic units described in the preceding lectures are rock units distinguished by: Magnetic characteristics Fossil content (Biostratigraphy) Seismic reflection characteristics To interpret Earth’s history, stratigraphic units must be related to geologic time. The ages of rock units must be known. Chronostratigraphy: Establishing the time relationship among rock units is called

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What are the principles of biostratigraphy?

What are the principles of biostratigraphy?

The characterization and correlation of rock units on the basis of their fossil content is called biostratigraphy. It is fundamentally different from a lithostratigraphic unit that is defined by the lithological properties of the rock. The concept of biostratigraphy is based on the principle that organisms have undergone successive changes throughout geologic time. Thus, any

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Hydrological properties of Rocks: Comprehensive Guide to Porosity, Specific Yield, and Storage Coefficient in Rocks

Hydrological properties of Rocks: Comprehensive Guide to Porosity, Specific Yield, and Storage Coefficient in Rocks

Hydrological properties of Rocks: Hydrological properties are the characteristics of rocks and soils that affect the movement, storage, and distribution of water within the Earth’s crust. These properties include porosity, permeability, specific yield, specific retention, and storativity, which determine the capacity of geological materials to store and transmit water. POROSITY (n) The bulk volume of

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Proximate and Ultimate Analysis of Coal: Comprehensive Guide to Coal Quality Parameters

Proximate and Ultimate Analysis of Coal: Comprehensive Guide to Coal Quality Parameters

Proximate analysis The most common analysis is proximate analysis. A proximate analysis is a common laboratory procedure to provide the fundamental composition of coal. It is used on coal during exploration, mining, and preparation. This analysis is also widely used for industrial purposes and for grading the coals.  Proximate analysis is a measure of the

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Lithostratigraphy: An Introduction to Earth’s Sedimentary Records

Lithostratigraphy: An Introduction to Earth’s Sedimentary Records

Lithostratigraphy Definition of Lithostratigraphy Lithostratigraphy is a branch of stratigraphy focused on the recognition, subdivision, and correlation of sedimentary rocks based on their lithology. Definition of Lithology Lithology involves the study and description of the physical characteristics of rocks, including: Lithostratigraphic Units Lithostratigraphic units are bodies of sedimentary, extrusive igneous, metasedimentary, or metavolcanic rock, defined

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