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le="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>le="FONT-FAMILY: Verdana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>Tectonic Deformation of Active Fault-Related Fold Belts in the North Piedmont of the l:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />laceName w:st="on">CentrallaceName> laceName w:st="on">TianshanlaceName> laceType w:st="on">MountainslaceType>, NW ntry-region w:st="on">lace w:st="on">Chinalace>ntry-region>le="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>l:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
le="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>The Distribution and Characteristics of Lacustrine Sedimentation from l:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />laceName w:st="on">AncientlaceName> laceName w:st="on">HighlaceName> laceName w:st="on">LevellaceName> laceType w:st="on">LakelaceType> at the North Foot oflace w:st="on"> Bayankala Mt., lace>le="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>lace w:st="on">Qinghai Province, ntry-region w:st="on">Chinantry-region>lace> l:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
