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cm 0cm 0pt" class=MsoNormal>ce="Times New Roman">Xiangshanxi Composite Cu-Ni—Ti-Fe Deposit Belongs to Comagmatic Evolution Productcii-font-family: ’Times New Roman’">：ce="Times New Roman">Evidences from Ore Microscopycii-font-family: ’Times New Roman’">，ce="Times New Roman">Zircon U-Pb Chronology and Petrological Geochemistry, Hamicii-font-family: ’Times New Roman’">，ce="Times New Roman">Xinjiangcii-font-family: ’Times New Roman’">，ce="Times New Roman">NW Chinace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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cm 0cm 0pt" class=MsoNormal>ce="Times New Roman">Xiangshanxi Composite Cu-Ni—Ti-Fe Deposit Belongs to Comagmatic Evolution Productcii-font-family: ’Times New Roman’">：ce="Times New Roman">Evidences from Ore Microscopycii-font-family: ’Times New Roman’">，ce="Times New Roman">Zircon U-Pb Chronology and Petrological Geochemistry, Hamicii-font-family: ’Times New Roman’">，ce="Times New Roman">Xinjiangcii-font-family: ’Times New Roman’">，ce="Times New Roman">NW Chinace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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cm 0cm 0pt" class=MsoNormal>ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>ce="Times New Roman">Study on Characteristics of Latest Mesozoic Paleock; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US>-ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>ce="Times New Roman">Structuresck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US> ce="Times New Roman">ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>in Front of ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">South Qilian Mountain, country-region w:st="on">Chinacountry-region>ce>ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt" lang=EN-US>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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cm 0cm 0pt" class=MsoNormal>ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>ce="Times New Roman">Study on Characteristics of Latest Mesozoic Paleock; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US>-ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>ce="Times New Roman">Structuresck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US> ce="Times New Roman">ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>in Front of ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">South Qilian Mountain, country-region w:st="on">Chinacountry-region>ce>ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt" lang=EN-US>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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cm 0cm 0pt" class=MsoNormal>ce="Times New Roman">ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>The Effect of the Reservoir Space in Carbonate Formationck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: Verdana" lang=EN-US> ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>by Fractureck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">：ce="Times New Roman">ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Taking the Ordovician Carbonate Formation ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>in Lungudong Region of ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">TarimceName> ceType w:st="on">BasinceType>ce> as an Exampleck; FONT-SIZE: 14pt" lang=EN-US>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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cm 0cm 0pt" class=MsoNormal>ce="Times New Roman">ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>The Effect of the Reservoir Space in Carbonate Formationck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: Verdana" lang=EN-US> ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>by Fractureck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">：ce="Times New Roman">ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Taking the Ordovician Carbonate Formation ck; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>in Lungudong Region of ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">TarimceName> ceType w:st="on">BasinceType>ce> as an Exampleck; FONT-SIZE: 14pt" lang=EN-US>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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