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<SPAN style="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>s New Roman">Timing of Initiation of Left-Lateral Slip along the Ailao Shan-Red River Shear Zone: Microstructural, Texture and Thermochronological Evidence from High Temperature Mylonites in space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:PlaceName w:st="on">Diancangshanst1:PlaceName> <st1:PlaceType w:st="on">Mountainsst1:PlaceType>, <st1:place w:st="on">SW Chinast1:place>
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style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>style="FONT-SIZE: 14pt" lang=EN-US>s New Roman">This paper studied the features of microstructures and mineral deformation in the high temperature mylonites collected from the Diancangshan region, and their deformation mechanism and mineral components. U-Pb zircons from a granitic high temperature mylonite were dated by SHRIMP. The results reveal that the main minerals such as feldspar, quartz and amphibole are characterized by high temperature crystalline ductile deformation and oriented growth under the condition of amphibolite facies, which provides evidencestyle="DISPLAY: none; COLOR: #0067b6; mso-hide: all"> for strike slip shearing deformation event.&nbsp;

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