Maymyo extension zone of shan scarp fault

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August undefined, 2024

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, … 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 ...

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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. 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 … david brown kcmo

Paleomagnetic constraints on the Mesozoic-Cenozoic …

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 … 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 … 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 … gas hob thermocouple replacement

Geology and Skarn Cu–Bi–Au Mineralization at ... - Semantic Scholar

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WebRiver Fault remained sinistral, but movement direction changed to dex-tral on the Three Pagodas–Mae Ping Faults. Dextral movement on the Sumatra Fault (Sm) began. At 15 Ma, movement on the Red River Fault ceased. Dextral movement on the Sumatra (Sm) and Sagaing (S) Faults was linked via extension in the Andaman Sea. At 5 Ma, there WebThe geology of Myanmar is shaped by dramatic, ongoing tectonic processes controlled by shifting tectonic components as the Indian plate slides northwards and towards Southeast Asia.[1] Myanmar spans across parts of three tectonic plates separated by north-trending faults. To the west, a highly oblique subduction zone separates the offshore Indian plate … david brown knivesWebShan 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 … david brown kansas city

"WebWe 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 … " - Maymyo extension zone of shan scarp fault

Maymyo extension zone of shan scarp fault

Diachronous cooling along the Mogok Metamorphic Belt (Shan scarp ...

Webconsequent fault scarp: ผาตามผารอยเลื่อน [ธรณีวิทยา๑๔ ม.ค. ๒๕๔๖]: composite fault scarp: ผารอยเลื่อนผสม [ธรณีวิทยา๑๔ ม.ค. ๒๕๔๖]: fault scarp: ผารอยเลื่อน [ธรณีวิทยา๑๔ ม.ค. ๒๕๔๖] 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 …

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Webits 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 ... WebSOE THURA TUN & WATKINSON Sagaing Fault 80. Immediately east of the Sagaing Fault between Mandalay and the Gulf of Mottama, the Shan Scarp . 81 fault zone forms the prominent eastern topographic margin of the Shan Plateau and appears to be 82 obliquely truncated by the Sagaing Fault (Bertrand & Rangin 2003) at about 23°N. …

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 … 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 …

Web10 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, … 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 …

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

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 david brown kpmgWebis 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 … david brown judgeWebA 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. gas hob trivetWebThe single most effective method for detecting and delineating fault scarps is to conduct aerial reconnaissance and remote sensing using low solar irradiation angles to produce shadows or highlights on scarps having slopes steeper than the irradiation angle of the sun. david brown judge ramsey countyWebAbstract: 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 … gas hob versus induction hobWeb16 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 … david brown lafourche parishWeb1 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 metamorphic and intrusive rocks that have been analyzed by 40Ar/39Ar step heating method. The 13 samples we analyzed provide Oligocene to Lower Miocene… View on … gas hob v induction hob