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Maymyo extension zone of shan scarp fault

Web31 okt. 2024 · However, due to the recurrence interval on each individual fault typically being several thousand years (Abdrakhmatov et al. 2016; Deev et al. 2016; Landgraf et al. 2016; Grützner et al. 2024; Patyniak et al. 2024), much of what is known about the earthquake history and slip rate of Tien Shan faults comes from palaeoseismic and … Web1 nov. 2024 · The slip rate along the west flank of the Stansbury Mountains varies from 0.04 to 0.2 mm/yr for time frames of 10 to >100 ka, with the most recent rupture on the …

Investigating paleoseismicity using fault scarp morphology of the ...

Web9 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 … WebMoreover, the study area is structurally unstable because it lies in the Shan Scarp Fault Zone. So, most of the landslide types occur in this area. ... occupying the whole of Pinmon Taung (4495’) and extended north up to Pyinnyaung scarp and south down beyond Sindaung (6015’). Brecciated dolomitic limestone, calcitic limestone, ... cvs beauty club expire https://thepreserveshop.com

Tectonics of the western margin of the Shan plateau (central …

Web5 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, … WebShan Scarp Shear zone and the Sagaing Fault. The fabric developments give information on the strain tensors transition of deeper ductile deformation to brittle deformation in shallow … 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 … cvs beauty commercial 2020

Variability in surface rupture between successive earthquakes on …

Category:Paleomagnetic constraints on the Mesozoic-Cenozoic …

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Maymyo extension zone of shan scarp fault

Tectonics of the western margin of the Shan plateau (central …

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 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.

Maymyo extension zone of shan scarp fault

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Web16 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 … WebAbstract: Cenozoic right-lateral shear between the eastern Indian margin and Eurasia is expressed by numerous N-S trending fault systems inboard of the Sunda trench, including the Sagaing Fault. The most easterly of these fault systems is the prominent ∼500 km long Kyaukkyan Fault, on the Shan Plateau. Myanmar’s largest recorded earthquake, Mw 7.7 …

Webis distributed across Myanmar in a platelet that extends from the western edge of the Shan Plateau in the east to the Andaman Trench in the west. In this platelet, deformation is … WebTibet, but that also major strike-slip faults had developed, including the left-lateral Ailao Shan-Red River fault (Fig. 1), along which crust has been extruded from the collision zone. Since that time, several views have been put forward based on disparate estimates on the amount of displacement along the Ailao Shan-Red River fault (Fig. 2 ...

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 ... WebWe 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

Web1 mei 2024 · The most easterly of these fault systems is the prominent ∼500 km long Kyaukkyan Fault, on the Shan Plateau. Myanmar’s largest recorded earthquake, M w …

WebThis fault was noticed early by Refs. [1-3] and later confirmed by several authors [4-9]. Moreover, some active faults also occurred in Myanmar, e.g. Sagaing dextral fault, Kyaukkyan fault, Kyaukme fault, Momeik fault, Shan scarp fault, Kabaw fault, Nama fault and Gwegyo fault, etc. Among them, Sagaing is the most active fault and cvs beauty club changes 2021Web1 aug. 2003 · Microtectonic analyses along the fault provide strong evidence for a dextral strike-slip component of motion. Unless full partitioning of the motion between the … cheapest hotel booking ratesWebWe first simulate fault scarp degradation using a nonlinear transport model to obtain the empirical relationship between scarp width and its evolution time. We then measure 68 … cvs beauty facebookWebAssuming 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 … cheapest hotel booking site topadslistWebits base. The greater height of the scarp crest here then is not the result of selective erosion, but of the uplift which probably occurred in Mid-Pliocene times. This displacement was limited to the fault-zone between Charade and Saulzet. . . . . . . .. FIGURE 2-The fault-scarp between the Grande Limagne and Plateaux des D6mes. For key see ... cvs beauty gift aprilWebShan 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 … cvs beauty instagramWeb10 nov. 2024 · The Kyaukkyan Fault bisects the western Shan Plateau, which is the southernmost promontory of Tibetan Plateau elevated topography (Fig. 1c). The fault lies within Sibumasu, a Gondwana-derived terrane accreted to Eurasia during the Paleozoic as part of the assembly SE Asia's continental core, termed Sundaland (e.g. ; Metcalfe, … cheapest hotel booking site india