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• W3142772407 endingPage "100055" @default.
• W3142772407 startingPage "100055" @default.
• W3142772407 abstract "Central Myanmar Basin (CMB) lies between the two major strike-slip faults: Sagaing Fault to the east and Kabaw Fault to the west. Central Volcanic Line of Myanmar emplaced en-echelon array of P-shears along the fault zone, which was active dextral as surrounding major faults at a low angle about 15° to the shear zone boundary. CMB was developed as strike-slip partitioned transpression model as proposed in this study. The transprsession tectonic is common with oblique convergence subduction as well as collision of India Plate to West Myanmar Block, especially effects on the CMB. Structural evidence are occurred as en-echelon folding and fracturing by satellite photos, field observation and 3D strain ellipsoid construction showing plane strain by pure shear upon ideal strike-slip with simple shear. In this study, two types of transpression distinguished as homogeneous and strike-slip partitioning which are developed within the frame of the strike-slip fault with progressive deformation. Under the condition of the strike-slip partitioned transpression, strain partitioning is distinctly occurred together with progressive deformation and reactivation of pre-existing structures such as cylindrical fold to double plunging fold, normal fault to oblique slip fault and positive flower structure. Deformation process related to the India Plate movement deduced the period of Late Miocene and Pliocene-Pleistocene based on the structural analysis in Rakhine Coastal region, western Myanmar. During the period between the Late Miocene to Pliocene-Pleistocene, pre-existing ophiolite zone in the Indo-Myanmar Ranges (IMR) was split up different zones by the Sagaing Fault displacement, accompanied to the West Myanmar Block movement with India Plate subduction. Accordance with the Sagaing Fault displacement and group of mud volcanoes shifting, the CMB moved northward about 450km with displacement rate 5–7cm per annum by the 45–50°convergent angle of India Plate collision to Eurasia Plate. Transpression deformation of northward compression was developed in the CMB, simultaneously on the other side transtension as pull-apart basin was formed by Andaman Sea opening at the south on the Sagaing Fault. During the Miocene time, collision of India Plate to Eurasia Plate was principal and caused the deformation at northern border the India, in which India Plate moved both in northwards and rotated anti-clockwise, whereas West Myanmar Block together with Sibumasu Block rotated clockwise becoming final closure of the northeasternmost Assam and Myanmar regions. During the Oligocene time, deposition of the shallow marine Barail formation in the Bengal Basin and shallow marine to continental shelf sequences in the CMB started as twin trough. This study provides the transpression deformation in the CMB and related regions during syn- and post-collision of India Plate to West Myanmar Block with position and kinematic structural interpretation." @default.
• W3142772407 created "2021-04-13" @default.
• W3142772407 creator A5015838081 @default.
• W3142772407 creator A5028598155 @default.
• W3142772407 creator A5052452617 @default.
• W3142772407 creator A5084050344 @default.
• W3142772407 date "2021-06-01" @default.
• W3142772407 modified "2023-10-18" @default.
• W3142772407 title "Dextral transpressional shearing and strike-slip partitioning developments in the Central Myanmar Basin during the collision between the India Plate and West Myanmar Block" @default.
• W3142772407 cites W1530018317 @default.
• W3142772407 cites W1606193387 @default.
• W3142772407 cites W1665325899 @default.
• W3142772407 cites W1675492458 @default.
• W3142772407 cites W1866635988 @default.
• W3142772407 cites W1965335989 @default.
• W3142772407 cites W1970922281 @default.
• W3142772407 cites W1983522549 @default.
• W3142772407 cites W1987649054 @default.
• W3142772407 cites W1988892793 @default.
• W3142772407 cites W1998671119 @default.
• W3142772407 cites W2003089534 @default.
• W3142772407 cites W2009038004 @default.
• W3142772407 cites W2010333805 @default.
• W3142772407 cites W2014987852 @default.
• W3142772407 cites W2016093409 @default.
• W3142772407 cites W2020646797 @default.
• W3142772407 cites W2020654422 @default.
• W3142772407 cites W2022909854 @default.
• W3142772407 cites W2025159153 @default.
• W3142772407 cites W2025963416 @default.
• W3142772407 cites W2027226653 @default.
• W3142772407 cites W2027603316 @default.
• W3142772407 cites W2027706900 @default.
• W3142772407 cites W2028775319 @default.
• W3142772407 cites W2031829064 @default.
• W3142772407 cites W2036279624 @default.
• W3142772407 cites W2038732125 @default.
• W3142772407 cites W2042326622 @default.
• W3142772407 cites W2053876360 @default.
• W3142772407 cites W2060925722 @default.
• W3142772407 cites W2061042341 @default.
• W3142772407 cites W2062802931 @default.
• W3142772407 cites W2064172431 @default.
• W3142772407 cites W2069716381 @default.
• W3142772407 cites W2076704383 @default.
• W3142772407 cites W2083171607 @default.
• W3142772407 cites W2089365850 @default.
• W3142772407 cites W2089635702 @default.
• W3142772407 cites W2092824442 @default.
• W3142772407 cites W2096884377 @default.
• W3142772407 cites W2103280364 @default.
• W3142772407 cites W2114115271 @default.
• W3142772407 cites W2138354656 @default.
• W3142772407 cites W2140771040 @default.
• W3142772407 cites W2155296909 @default.
• W3142772407 cites W2160412587 @default.
• W3142772407 cites W2168928513 @default.
• W3142772407 cites W2188328904 @default.
• W3142772407 cites W2324192404 @default.
• W3142772407 cites W2325715544 @default.
• W3142772407 cites W2332870841 @default.
• W3142772407 cites W2336276303 @default.
• W3142772407 cites W2344174229 @default.
• W3142772407 cites W2462808959 @default.
• W3142772407 cites W2521553249 @default.
• W3142772407 cites W2585322630 @default.
• W3142772407 cites W2596781312 @default.
• W3142772407 cites W2745517307 @default.
• W3142772407 cites W2751055046 @default.
• W3142772407 cites W2768426907 @default.
• W3142772407 cites W2769012639 @default.
• W3142772407 cites W2769104712 @default.
• W3142772407 cites W2769816252 @default.
• W3142772407 cites W2769943695 @default.
• W3142772407 cites W2770340404 @default.
• W3142772407 cites W2770877352 @default.
• W3142772407 cites W2789762075 @default.
• W3142772407 cites W2911409070 @default.
• W3142772407 cites W2937294608 @default.
• W3142772407 cites W2941893226 @default.
• W3142772407 cites W2967421299 @default.
• W3142772407 cites W2968887791 @default.
• W3142772407 cites W2972650086 @default.
• W3142772407 cites W2988897983 @default.
• W3142772407 cites W2991009594 @default.
• W3142772407 cites W3004202550 @default.
• W3142772407 cites W3012024621 @default.
• W3142772407 cites W3037091909 @default.
• W3142772407 cites W336368833 @default.
• W3142772407 cites W4240586711 @default.
• W3142772407 cites W4245867505 @default.
• W3142772407 doi "https://doi.org/10.1016/j.jaesx.2021.100055" @default.
• W3142772407 hasPublicationYear "2021" @default.
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