Shan Scarp. The topographic boundary separating the Myanmar Central Basin (MCB) and the Shan Plateau (or Eastern Highland) is referred as the Shan Scarp. The abrupt elevation over a short distance (up to 1.8 km over few km) harbors the trace of reverse faults and largely overturned folds. Visa mer The 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. Myanmar spans across parts of three Visa mer The tectonic setting of Myanmar consists of a highly oblique convergence on the western boundary, a dextral (right lateral) strike-slip fault in the centre of Myanmar defining the Burma-Sunda boundary and the spreading of Andaman Sea Ridge in the south. Visa mer Mineral belts Myanmar hosts a variety of ore-deposits with economic significance and global recognition. It is a global source of true jade and produces some of the world's finest rubies, with mines in the Mogok Valley providing … Visa mer Myanmar is classified into three physiographical regions, each region spans over Myanmar in near NS direction, from west to east is: … Visa mer Indo-Burman Range The Indo-Burman Range is a sedimentary belt mainly consisted of Cenozoic flysch sediments and a core of Mesozoic ophiolites dated … Visa mer Myanmar lies on the boundary of three tectonic plates (India, Burma-micro and Sunda Plate), thus its geological evolution is highly dependent on the plate tectonic events in this region. … Visa mer • Myanmar portal Visa mer

Pull-apart development at overlapping fault tips

Webb1 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 … WebbTogether with the adjacent Mergui Slate Belt these rocks lie to the west of the Shan Scarp and the Paung Laung-Mawchi Zone, interpreted by Mitchell et al. (2012) as a possible … list wealthiest americans

Cenozoic metamorphism along the Shan Scarp (Myanmar): …

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