Plio-Pleistocene to Recent tectonostratigraphic evolution of the Lalmai anticline in the western Indo-Burman Range (Bangladesh): insights from lithofacies analysis and structural synthesis

• Published in: Arabian journal of geosciences 2021-03, Vol.14 (5), Article 392
• Main Authors: Abdullah, Rashed, Sayem, Abu Sadat Md, Yeasmin, Rumana, Rahman, Mohammad Mashiur, Bari, Zahidul, Khanam, Farida
• Format: Article
• Language: English
• Subjects: Anticlines; Belts; Cenozoic; Clay; Crustal shortening; Earth and Environmental Science; Earth science; Earth Sciences; Escarpments; Evolution; Formations; Identification; Lithofacies; Mudstone; Original Paper; Pleistocene; Sandstone; Sedimentary facies; Sedimentary rocks; Shale; Subduction; Subduction (geology); Tectonics
• ISSN: 1866-7511; 1866-7538
• DOI: 10.1007/s12517-021-06741-z

The Lalmai anticline is one of the westernmost structures within the Eastern Fold Belt of the Bengal Basin that has surficial expression. The tectonic evolution of the Eastern Fold Belt is directly linked with the development of the Indo-Burman Range in response to the late Cenozoic convergence between the Indian and Burmese plates. However, very little is known about the Plio-Pleistocene to Recent tectonic evolution of the Lalmai anticline in the context of regional tectonics. Therefore, this research is aimed at lucid understand the Plio-Pleistocene to Recent tectonostratigraphic evolution of the Lalmai anticline based on detailed lithofacies and structural observations. Results show that Plio-Pleistocene Dupitila and Pleistocene Madhupur Clay formations are exposed in the Lalmai area. Based on sedimentary texture and structures, a total of six prominent lithofacies types have been identified. These are trough cross-stratified sandstone (S t ), planar cross-stratified sandstone (S p ), parallel laminated sandstone (S l ), massive sandstone (S m ), laminated shale (F l ), and mudstone (F m ) facies. The facies characteristics indicate a possible fluvial depositional environment for both the formations. Structural mapping shows that the bedding surfaces are nearly horizontal. Based on the missing of strata (both the Dupitila and Madhupur Clay formations) and presence of a fault escarpment, a N-S trending east-dipping reverse fault (namely, the Mainamati Fault) has been identified on the western margin of the Lalmai anticline. The tectonostratigraphic evolutionary models show that the last major structural activation along this Mainamati Fault can be linked to late Pleistocene to Recent time. This structural activation was possibly controlled by the latest ongoing E-W crustal shortening in response to the Indo-Burman subduction processes to the far east.