中文地质文摘分类法(404)
结晶学与矿物学(2)
地球化学(38)
古生物(2)
地层学与地史学(2)
区域地质学(22)
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地质普查勘探方法(2)
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在“中国地质文献-英文”中,命中:404条,耗时:0.014993 秒

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt&quot; lang=EN-US>ce=&quot;Times New Roman&quot;>Application of Remote Sensing Technique in the Mapping of Cenozoic Geology of the ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ce w:st=&quot;on&quot;>ceName w:st=&quot;on&quot;>EastceName> ceName w:st=&quot;on&quot;>KunlunceName> ceType w:st=&quot;on&quot;>MountainsceType>ce>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt&quot; lang=EN-US>ce=&quot;Times New Roman&quot;>Application of Remote Sensing Technique in the Mapping of Cenozoic Geology of the ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ce w:st=&quot;on&quot;>ceName w:st=&quot;on&quot;>EastceName> ceName w:st=&quot;on&quot;>KunlunceName> ceType w:st=&quot;on&quot;>MountainsceType>ce>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Petroleum Geological Features of ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ceName w:st=&quot;on&quot;>UpperceName> ceName w:st=&quot;on&quot;>MagdalenaceName> ceType w:st=&quot;on&quot;>BasinceType> in country-region w:st=&quot;on&quot;>ce w:st=&quot;on&quot;>Colombiace>country-region>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Petroleum Geological Features of ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ceName w:st=&quot;on&quot;>UpperceName> ceName w:st=&quot;on&quot;>MagdalenaceName> ceType w:st=&quot;on&quot;>BasinceType> in country-region w:st=&quot;on&quot;>ce w:st=&quot;on&quot;>Colombiace>country-region>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Conchostracan Biostratigraphy of the Dadianzi Formation in the ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ceName w:st=&quot;on&quot;>LuanpingceName> ceType w:st=&quot;on&quot;>BasinceType>, Northern ce w:st=&quot;on&quot;>ot;on&quot;>Hebei Province, country-region w:st=&quot;on&quot;>Chinacountry-region>ce> and the Boundary of Continental Jurassic and Cretaceous Strataml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Conchostracan Biostratigraphy of the Dadianzi Formation in the ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ceName w:st=&quot;on&quot;>LuanpingceName> ceType w:st=&quot;on&quot;>BasinceType>, Northern ce w:st=&quot;on&quot;>ot;on&quot;>Hebei Province, country-region w:st=&quot;on&quot;>Chinacountry-region>ce> and the Boundary of Continental Jurassic and Cretaceous Strataml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Geology of Porphyry and Skarn Type Copper Polymetallic Deposits in the Southern Margin of ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ce w:st=&quot;on&quot;>ceName w:st=&quot;on&quot;>QaidamceName> ceType w:st=&quot;on&quot;>BasinceType>ce>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Geology of Porphyry and Skarn Type Copper Polymetallic Deposits in the Southern Margin of ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ce w:st=&quot;on&quot;>ceName w:st=&quot;on&quot;>QaidamceName> ceType w:st=&quot;on&quot;>BasinceType>ce>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Palynological Assemblage of Eocene-Oligocene Pollen and Their Biostratigraphic Correlation in Dahonggou, Daqaidam Area, ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ce w:st=&quot;on&quot;>ceName w:st=&quot;on&quot;>QaidamceName> ceType w:st=&quot;on&quot;>BasinceType>ce>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>Palynological Assemblage of Eocene-Oligocene Pollen and Their Biostratigraphic Correlation in Dahonggou, Daqaidam Area, ml:namespace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ce w:st=&quot;on&quot;>ceName w:st=&quot;on&quot;>QaidamceName> ceType w:st=&quot;on&quot;>BasinceType>ce>ml:namespace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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