Provenance and Depositional Setting of Black Shales from the Dhalbhum Formation, North Singhbhum Mobile Belt, Eastern India
Authors
-
Department of Geology, Aligarh Muslim University, Aligarh – 202 002
Naurin Khan Malik -
Department of Geology, Aligarh Muslim University, Aligarh – 202 002
Shabber Habib Alvi
DOI:
https://doi.org/10.1007/s12594-021-1754-7Keywords:
No KeywordsAbstract
The Paleoproterozoic black shales of the Dhalbhum Formation exposed to the north of the Dalma metavolcanic suite is comprised of siliciclastic rocks and a minor amount of carbonaceous rocks. Geochemical studies were carried out to study the provenance and depositional setting of black shales. The average values of Co, V, U, and Cr/V (1.29) and Ni/Co (2.77) ratios in the black shales of Dhalbhum Formation are higher as compared to those of the Post-Archean Australian shale (PAAS) values (Cr/V=0.73, Ni/Co= 2.39). The chondrite normalized rare earth elements (REEs) patterns, indicate the enrichment in LREE (SLREE/HREE =10.73) and flat HREEs. The immobile element ratios Th/Sc (1.14), Th/Co (1.120), Cr/Th (16.161), and La/Sc (2.80) of studied samples indicate that sediments were derived from felsic rocks, which is also corroborated by La-Th-Sc ternary diagram. The sediments deposited at the active continental margin generally show REE pattern intermediate between a typical andesite and PAAS. A continental margin tectonic setting is distinguished by La-Th-Sc, Th-Co-Zr/10 and Th-Sc-Zr/10, which is further corroborated by Yb vs Th/Ta diagram where the samples plot in the field of active continental margin.
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