Back to Search Start Over

Geochemistry and detrital zircon U–Pb dating of Pliocene-Pleistocene sandstones of the Chittagong Tripura Fold Belt (Bangladesh): Implications for provenance.

Authors :
Rahman, M. Julleh Jalalur
Xiao, Wenjiao
Hossain, Md Sakawat
Yeasmin, Rumana
Sayem, Abu Sadat Md
Ao, Songjian
Yang, Lei
Abdullah, Rashed
Dina, Nafisa Tamanaya
Source :
Gondwana Research; Feb2020, Vol. 78, p278-290, 13p
Publication Year :
2020

Abstract

The Bengal Basin originated during the collision of India with Eurasia and Burma. The provenance analysis of the Chittagong Tripura Fold Belt (CTFB), which is the folded eastern flank of the Bengal Basin as well as the Neogene belt of the Indo-Burman Ranges (IBR) is key to better understand the possible sources of sediment input from the complex interplay of the Indian, Eurasian and Burma plates. We report new whole rock geochemical and detrital zircon U–Pb data from the upper Neogene sandstones of Tipam-Dupi Tila formations (Pliocene to Plio-Plestocene succession) from the CTFB. Detrital zircon U–Pb age spectra show three predominant peaks at <200 Ma, 480–650, ∼800–1000 Ma. The geochemical discriminations and elemental ratios of Eu/Eu* (∼0.70), La/Sc (∼16.13), La/Co (∼15.76), Th/Sc (∼2.95), La/Th (∼5.67), Th/Co (∼2.87), Cr/Th (∼4.63) as well as Chondrite-normalized REE patterns with flat HREE, LREE enrichment, and negative Eu anomalies for the Tipam and Dupi Tila formations are suggestive of a dominantly felsic source area experiencing moderate to intensive chemical weathering (Chemical index of alteration, CIA - 57 to 81) and have a recycled provenance orogen related to active continental or passive margin settings. Integrated geochemical and zircon U–Pb studies reveal that the main sediment input might have been from the Himalayan orogen with significant arc-derived detritus, possibly from the Gangdese arc as well as from the Burma magmatic arc. Image 1 • Provenance of Plio-Pleistocene sedimentary rocks has been established for the Chittagong Tripura Fold Belt, Bengal Basin using whole rock geochemistry and U–Pb detrital geochronology. • The sedimentary rocks were derived dominantly from felsic sources rocks. • Sediments were sourced predominantly from the Himalaya and additional young zircons (<200 Ma) from the Burma magmatic arc. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
1342937X
Volume :
78
Database :
Supplemental Index
Journal :
Gondwana Research
Publication Type :
Academic Journal
Accession number :
141730485
Full Text :
https://doi.org/10.1016/j.gr.2019.07.018