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ARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>Tectonic Deformation of Active Fault-Related Fold Belts in the North Piedmont of the namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />aceName w:st="on">CentralaceName> aceName w:st="on">TianshanaceName> aceType w:st="on">MountainsaceType>, NW ntry-region w:st="on">ace w:st="on">Chinaace>ntry-region>ack; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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ARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>ana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>Glacial Advance in the Qinghai-Tibet Plateau and namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">PeripheralaceName> aceType w:st="on">MountainsaceType>ace> during the MID-MIS 3ack; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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