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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

Permalink : http://hdl.handle.net/20.500.12678/0000000476
1d9ff9e5-00ed-4dc3-894a-1fb447713be7
d91c00a3-07ea-46d1-97d1-c4f6f1434ef6
Preview
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Origin Origin and time of Major Structure in Anisakan – Kangyigon Area,.pdf (632.7 kB)
sha256: d071e3f93225f8c8f6a2b75d7d0a58fc81d18c356a4cb3bd1e172d9cfadceb96
Publication type Journal article
Upload Type Publication
Title
Origin and time of Major Structure in Anisakan – Kangyigon Area, Pyinoolwin Township: an emphasis on the analysis of minor structure
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
Files 633 Kb
Available
2020-05-05
application/pdf
preview
application/pdf
open_access
Origin and time of Major Structure in Anisakan – Kangyigon Area,.pdf

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