quot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>quot;COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt" lang=EN-US>quot;Times New Roman">Application of Remote Sensing Technique in the Mapping of Cenozoic Geology of the quot;urn:schemas-microsoft-com:office:smarttags" />quot;on">quot;on">East quot;on">Kunlun quot;on">Mountainsquot;urn:schemas-microsoft-com:office:office" />

详细信息   
摘要

quot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>quot;FONT-SIZE: 14pt" lang=EN-US>quot;Times New Roman">According to the color variations of different geological bodies in the same wave band or the same geological body in different wave bands, a close geological interpretation has been made for the ETM images from the quot;urn:schemas-microsoft-com:office:smarttags" />quot;on">East quot;on">Wenquan quot;on">Basin of the east quot;on">quot;on">Kunlun quot;on">Mountains, resulting in the establishment of interpretation makers for the Cenozoic strata and new structures. The interpretation allows to accurately define the Cenozoic strata boundaries and Cenozoic fault locations on the ETM images. The Cenozoic strata in the mapping area can be divided into 10 mapping units based on the field survey. The Cenozoic faults include nearly NW left-lateral strike-slip faults and nearly NWW thrust nappe structures.quot;FONT-SIZE: 14pt; mso-font-kerning: 0pt" lang=EN-US>quot;urn:schemas-microsoft-com:office:office" />

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