The research area is situated within the northern adjacent part of the Momeik Town. It is mainly composed of metamorphic (metapelite, metacarbonate and metaigneous) and associated igneous rocks. The present work deals to describe the petrographic criteria of structural deformation and to interpret the tectonic evolution of the study area. The investigations of numerous deformational criteria observed in various units of the study area point out that the research area might have been encountered four different styles of deformation during Tertiary period. These are (i) E-W compressional deformation (Eocene to Oligocene), (ii) NNW-SSE ductile-extensional deformation (Oligocene to Early Miocene), (iii) brittle-ductile deformation (Early to Mid...
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by m...
4siMultiple episodes of deformation during the tectonic evolution of orogenic belts and ancient subd...
The Biluoxueshan deformation zone is an Early Eocene dextral transpressive zone located around the E...
The research area is situated about 7 miles from Momeik and 8 miles north west of Mogok in the boun...
The research area is situated within the northern adjacent part of the Momeik Town. It is mainly com...
Lack of work focusing on deformation mechanism has been undertaken in the Late Tertiary sequence dur...
International audienceThe paper is concerned with the kinematics of the major faults, their pattern,...
Deformation processes in the Shimanto Subduction Complex in the eastern Hata Peninsula, SW Japan hav...
The goal of this study was to identify and describe different microstructures observed in samples fr...
The research area is situated within the northern adjacent part of the Momeik Town. It is constitut...
The research area, Hngetmi Taung is located about 11 miles southeast of Pyawbwe, so it is easily acc...
The c. 500-km-long Mae Ping fault zone trends NW–SE across Thailand into eastern Myanmar and has pro...
A 10 km wide coastal strip of the Aileu Formation was mapped in detail. This section of the north c...
Lambolemo Village is geomorphologically dominated by hilly slopes morphology. Lithology in the form ...
Subject of investigation: Central Cola Peninsula granulitic gneiss region. Purpose of the work: reve...
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by m...
4siMultiple episodes of deformation during the tectonic evolution of orogenic belts and ancient subd...
The Biluoxueshan deformation zone is an Early Eocene dextral transpressive zone located around the E...
The research area is situated about 7 miles from Momeik and 8 miles north west of Mogok in the boun...
The research area is situated within the northern adjacent part of the Momeik Town. It is mainly com...
Lack of work focusing on deformation mechanism has been undertaken in the Late Tertiary sequence dur...
International audienceThe paper is concerned with the kinematics of the major faults, their pattern,...
Deformation processes in the Shimanto Subduction Complex in the eastern Hata Peninsula, SW Japan hav...
The goal of this study was to identify and describe different microstructures observed in samples fr...
The research area is situated within the northern adjacent part of the Momeik Town. It is constitut...
The research area, Hngetmi Taung is located about 11 miles southeast of Pyawbwe, so it is easily acc...
The c. 500-km-long Mae Ping fault zone trends NW–SE across Thailand into eastern Myanmar and has pro...
A 10 km wide coastal strip of the Aileu Formation was mapped in detail. This section of the north c...
Lambolemo Village is geomorphologically dominated by hilly slopes morphology. Lithology in the form ...
Subject of investigation: Central Cola Peninsula granulitic gneiss region. Purpose of the work: reve...
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by m...
4siMultiple episodes of deformation during the tectonic evolution of orogenic belts and ancient subd...
The Biluoxueshan deformation zone is an Early Eocene dextral transpressive zone located around the E...