2024 Maymyo extension zone of shan scarp fault

Maymyo extension zone of shan scarp fault

Author: cmtf

August undefined, 2024

Web19 nov. 2003 · On the contrary the Shan Scarp fault is rather linear, and dies out southward at the junction with the Three Pagodas fault. South of Mandalay the Shan Scarp fault foothills are formed by faulted Cenozoic gneissic domes. Metamorphism was dated between 25 and 14 Ma, and pervasive N160°E trending lineations are interpreted as steady state ... WebIn the 21 north the fault terminates within the complex intersection between the sinistral Kyaukme and Momeik 22 faults, the largely inactive Shan Scarp Fault Zone ... Fault (Myint Lwin Thein 1973) and the Taunggyi Fault (Bender 1983) 41 have been associated with a wider Kyaukkyan fault zone. Around the centenary of the Maymyo 42 earthquake ...

A: Simplified geologic map of Shuang Hu region. Locations of …

Web1 apr. 1999 · The Mogok metamorphic belt, exposed along the N-S trending Shan scarp and Sagaing fault, in the eastern part of Myanmar, has been regarded as Paleozoic to … WebRequest PDF On Jan 1, 2014, A.D.B. Cook published Human insecurity and displacement along myanmar’s borders Find, read and cite all the research you need on ResearchGate mohawk boardwalk collection

Human insecurity and displacement along myanmar’s borders

Web27 aug. 2015 · Shan Scarp Fault Zone is the prominent topographic feature of the Shan Plateau and appears to be obliquely truncated by the Sagaing Fault in the west. Shan … WebThe Shan Hills (Burmese: ရှမ်းရိုးမ; Shan Yoma), also known as Shan Highland, is a vast mountainous zone that extends through Yunnan to Myanmar and Thailand.The whole region is made up of numerous peaks separated mostly by narrow valleys, as well as a few broader intermontane basins.The ranges in the area are aligned in such a way that they … WebA fault scarp is a small step or offset on the ground surface where one side of a fault has moved vertically with respect to the other. [1] It is the topographic expression of faulting attributed to the displacement of the land surface by movement along faults. mohawk bold thinking

Evidence of Quaternary and recent activity along the Kyaukkyan …

Shan Hills - Wikipedia

WebMyanmarʼs largest recorded earthquake (M 8.0) occurred on the Kyaukkyan Fault close to Maymyo in 1912, which caused extensive damage in Mandalay and across the Shan states (Brown, 1917). Despite this, the fault zone is poorly known. There have been limited detailed mapping and structural studies, and the faultʼs significance, origin and Web1 aug. 2003 · A transtensionnal regime that generated NNW–SSE ductile stretching structures and N70E striking brittle normal faults was followed by a transpressionnal regime that generated right-lateral strike-slip structures; first, the Shan scarp and second, the Sagaing fault. This change in tectonic regime is summarized on Fig. 13. mohawk boardwalk collective bleached linenWeb26 mrt. 2024 · Faulting may produce a single strand, or the strain (deformation) may be distributed across a zone of closely spaced faults; the width of these fault zones ranges from a few centimetres to many 10s of metres. The development of fault zones depends to a large extent on the competency or strength of the rock; they are more common in weak … mohawk block it toner

"WebThe metallogenic provinces of Myanmar defined by the easterly-dipping Andaman subduction Myanmar has been variously divided into a number of zone, continues onshore to the western margin of the metallogenic … " - Maymyo extension zone of shan scarp fault

Maymyo extension zone of shan scarp fault

Cenozoic metamorphism along the Shan Scarp …

Web1 apr. 1999 · New observations in the Shan scarp area, close to the Sagaing fault, from Thaton in the south to Mandalay in the north, allowed us to collect samples of high grade … WebAssuming coeval slip at the present rates on the Haiyuan and Gulang Faults in the last 8 Ma would bring the cumulative left-lateral displacement between NE Tibet and the Ala Shan Platform to about 120 km consistent with the 95 ± 15 km offset of the Yellow River across the Haiyuan Fault, but many times the offset (≈16 km) inferred on one recent strand of …

Did you know?

Web8 jun. 2024 · Figure 3.5. 1: Faulting that occurs in the crust under tensional stress. Grabens, horsts, and half-grabens are blocks of crust or rock bounded by normal faults (see Chapter 2 ). Grabens drop down relative to adjacent blocks and create valleys. Horsts rise up relative to adjacent down-dropped blocks and become areas of higher topography.

WebShan Scarp Fault Zone is the prominent topographic feature of the Shan Plateau and appears to be obliquely truncated by the Sagaing Fault in the west. Shan Scarp Fault … WebThe Shan scarp-Sagaing fault area displays numerous outcrops of metamorphic and intrusive rocks, which belong to a sigmoidal metamorphic belt referred to by Chhibber …

WebThe northeast extension normal faults can be interpreted that accommodating the lateral and vertical movement of the crust in the southern Central Range. Based on … Web1 apr. 1999 · New observations in the Shan scarp area, close to the Sagaing fault, from Thaton in the south to Mandalay in the north, allowed us to collect samples of high grade …

Webdistance of 36 miles (about 58 km). Moreover he traced this active fault zone on air photos and topo maps up to northern Myanmar border and southwards until the fault enters the Andaman Sea (Win Swe 1970 & 1981). He named it Sagaing Fault. He differentiated it from the Shan Boundary or Shan Scarp Fault.

WebA shear-zone origin for the Uluda Massif is indicated by: (1) its location at the tip of the active Eskiehir oblique-slip fault, (2) pervasive subhorizontal mineral lineation in the gneisses with a right-lateral sense of slip, (3) … mohawk body shopWeb16 aug. 2024 · The Shwe Min Bon Cu–Au skarn deposit lies within one of the largest Au–Cu belts in Myanmar. The deposit is situated along the Shan scarp zone, which marks the boundary between the Myanmar central basin to the west and the Shan plateau to the east. The Shwe Min Bon deposit comprises skarn‐type metasomatic alteration, and the Cu–Au … mohawk blue bath rugsWebFour sketches showing progressive evolution of a fault scarp (top) to a featureless plain, and then to renewed relief. The fourth (lowest) diagram shows how renewed faulting … mohawk boardwalk collective gulf sandWebWe present new observations and new mineral ages (eight by the 40 Ar/ 39 Ar and nine by the 40 K-40 Ar methods) from high grade metamorphic and foliated intrusive rocks collected along the Mogok Metamorphic Belt of central Myanmar, that complete mohawk boardwalk collective sand duneWeb9 apr. 2024 · The red open arrows on the horizontal plane mark the pressure direction on each unit. In the vertical section, the EIBRSZ, Sagaing Fault (SF) and Shan Scarp Fault … mohawk boardwalk collective outerbanksWeb5 mei 2015 · This tectonic transformation has caused deformation to transfer from both the Pamir's eastern margin and its northwestern extension to the Pamir-Tian Shan convergent zone, which includes both the Pamir Frontal Thrust, a fault formed by northward propagation of the Pamir with a Quaternary shortening rate of ~6–7 mm/a [Li et al., 2012, … mohawk boswell cool grey tileWebWe present new data and interpretations on the Neogene tectonics of the Shan scarp area (central Myanmar) and its relationship with the India-Indochina oblique convergence. We … mohawk boardwalk collective beachwood