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  1. Yadanabon University
  2. Department of Geology

Origin and time of Major Structure in Anisakan – Kangyigon Area, Pyinoolwin Township: an emphasis on the analysis of minor structure

http://hdl.handle.net/20.500.12678/0000000476
http://hdl.handle.net/20.500.12678/0000000476
1d9ff9e5-00ed-4dc3-894a-1fb447713be7
d91c00a3-07ea-46d1-97d1-c4f6f1434ef6
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Origin Origin and time of Major Structure in Anisakan – Kangyigon Area,.pdf (633 Kb)
Publication type
Journal article
Upload type
Publication
Title
Title Origin and time of Major Structure in Anisakan – Kangyigon Area, Pyinoolwin Township: an emphasis on the analysis of minor structure
Language en
Publication date 2019
Authors
Khaing Khaing San
Description
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.
Keywords
structure
Identifier https://oar.ydbu.edu.mm/handle/123456789/295
Journal articles
1
Yadanabon University Research Journal
10
Conference papaers
Books/reports/chapters
Thesis/dissertations
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