2026-05-01T14:15:29Z https://meral.edu.mm/oai

oai:meral.edu.mm:recid/476 2021-12-13T00:54:35Z 1582963788001:1582966668038 user-ydbu

Origin and time of Major Structure in Anisakan – Kangyigon Area, Pyinoolwin Township: an emphasis on the analysis of minor structure Khaing Khaing San The Anisakan – Kangyigon area is mainly composed of the Paleozoic sequence of Ordovician to Early Triassic rock units. This area is a fairly rugged terrain shaped by various geological processes especially folding, faulting, denudation and karstic processes. The whole structure is overturned anticline and syncline nearly NNE – SSW and NE – SW trend. All major faults are cut across the regional tectonic and topographic trend running nearly E – W. This area is structurally very complicated which is disturbed by the Shan – Burma Boundary fault zone. The present work deals with the interpretation of major structure and tectonic effect of the study area based on the analysis of minor parasitic folds in Nyaungbaw Formation. These folds are interpreted as shear folds which can identify the major shear strike-slip faults and estimate the time and setting of the major structure in this area. 2019 http://hdl.handle.net/20.500.12678/0000000476 https://meral.edu.mm/records/476