Mineralogical and Geochemical Behavior of Sediments Solely Derived from Bundelkhand Granitic Complex, Central India: Implications to Provenance and Source Rock Weathering

Kanhaiya, S.; Singh, Birendra; Singh, S. K.

doi:10.1134/s0016702918120054

Cited by 17 publications

(5 citation statements)

References 40 publications

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“…Therefore, the geochemistry of clastic rocks appears as a useful tool for reconstructing provenance, paleoweathering, as well as tectonic regime and paleoenvironmental conditions prevailing during deposition. For this purpose, major, trace and REEs and their elemental ratios can be considered as sensitive recorders, and are commonly used to understand the sedimentation condition of basin infill ( Bathia, 1983 ; Roser and Korsch, 1986 ; Mc Lennan and Taylor, 1991 ; Mc Lennan et al., 1993 ; Condie, 1993 ; Nesbit et al., 1996 ; Fedo et al., 1997 ; 2002 ; Singh, 2013 ; Kanhaiya et al., 2018 ).…”

Section: Discussionmentioning

confidence: 99%

Provenance, paleoweathering, depositional setting and paleoclimatic constraints of cretaceous and neogene deposits of The Mamfe Basin, southwest Cameroon

Bilobe

Eyong

Samankassou

2022

Heliyon

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Section: Discussionmentioning

confidence: 99%

Provenance, paleoweathering, depositional setting and paleoclimatic constraints of cretaceous and neogene deposits of The Mamfe Basin, southwest Cameroon

Bilobe

Eyong

Samankassou

2022

Heliyon

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“…Therefore, the geochemistry of clastic rocks appears as a useful tool for reconstructing provenance, paleoweathering, as well as tectonic regime and paleoenvironmental conditions prevailing during deposition. For this purpose, major, trace and REEs and their elemental ratios can be considered as sensitive recorders, and are commonly used to understand the sedimentation condition of basin infill (Bathia, 1983;Roser and Korsch, 1986;Mc Lennan and Taylor, 1991;Mc Lennan et al, 1993;Condie, 1993;Nesbit et al, 1996;Fedo et al, 1997;Singh, 2013;Kanhaiya et al, 2018).…”

Section: Discussionmentioning

confidence: 99%

Provenance, Paleoweathering, Depositional Setting and Paleoclimatic Constraints of Cretaceous and Neogene Deposits of the Mamfe Basin, Southwest Cameroon

Bilobe

Eyong²,

Samankassou³

2022

SSRN Journal

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“…On the contrary, the transition elements (Co, Ni, and V) are immobile during weathering, and are compatible in magmatic processes. Therefore, Co is highly concentrated in ultramafic and mafic source rocks than felsic rocks [107], and thus mirror the chemistry of their source rocks [108]. Presently, no sediment contribution from oceanic island arc setting is indicated; however, to verify this, the concentration of V and Ni provides valuable information.…”

Section: La/th Versus Hf(ppm) and Ti/zr Versus La/sc And Nb/la Versus (La/sm)n Plotsmentioning

confidence: 99%

Multi-Proxy Provenance Analyses of the Kingriali and Datta Formations (Triassic–Jurassic Transition): Evidence for Westward Extension of the Neo-Tethys Passive Margin from the Salt Range (Pakistan)

et al. 2021

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The Salt Range, in Pakistan, preserves an insightful sedimentary record of passive margin dynamics along the NW margin of the Indian Plate during the Mesozoic. This study develops provenance analyses of the Upper Triassic (Kingriali Formation) to Lower Jurassic (Datta Formation) siliciclastics from the Salt and Trans Indus ranges based on outcrop analysis, petrography, bulk sediment elemental geochemistry, and heavy-mineral data. The sandstones are texturally and compositionally mature quartz arenites and the conglomerates are quartz rich oligomictic conglomerates. Geochemical proxies support sediment derivation from acidic sources and deposition under a passive margin setting. The transparent heavy mineral suite consists of zircon, tourmaline, and rutile (ZTR) with minor staurolite in the Triassic strata that diminishes in the Jurassic strata. Together, these data indicate that the sediments were supplied by erosion of the older siliciclastics of the eastern Salt Range and adjoining areas of the Indian Plate. The proportion of recycled component exceeds the previous literature estimates for direct sediment derivation from the Indian Shield. A possible increase in detritus supply from the Salt Range itself indicates notably different conditions of sediment generation, during the Triassic–Jurassic transition. The present results suggest that, during the Triassic–Jurassic transition in the Salt Range, direct sediment supply from the Indian Shield was probably reduced and the Triassic and older siliciclastics were exhumed on an elevated passive margin and reworked by a locally established fluvio-deltaic system. The sediment transport had a north-northwestward trend parallel to the northwestern Tethyan margin of the Indian Plate and normal to its opening axis. During the Late Triassic, hot and arid hot-house palaeoclimate prevailed in the area that gave way to a hot and humid greenhouse palaeoclimate across the Triassic–Jurassic Boundary. Sedimentological similarity between the Salt Range succession and the Neo-Tethyan succession exposed to the east on the northern Indian passive Neo-Tethyan margin suggests a possible westward extension of this margin.

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Mineralogical and Geochemical Behavior of Sediments Solely Derived from Bundelkhand Granitic Complex, Central India: Implications to Provenance and Source Rock Weathering

Cited by 17 publications

References 40 publications

Provenance, paleoweathering, depositional setting and paleoclimatic constraints of cretaceous and neogene deposits of The Mamfe Basin, southwest Cameroon

Provenance, paleoweathering, depositional setting and paleoclimatic constraints of cretaceous and neogene deposits of The Mamfe Basin, southwest Cameroon

Provenance, Paleoweathering, Depositional Setting and Paleoclimatic Constraints of Cretaceous and Neogene Deposits of the Mamfe Basin, Southwest Cameroon

Multi-Proxy Provenance Analyses of the Kingriali and Datta Formations (Triassic–Jurassic Transition): Evidence for Westward Extension of the Neo-Tethys Passive Margin from the Salt Range (Pakistan)

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