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kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Depositional Environment of the Tongziyan Formationkerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US> kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>of Dinfengshan Coal Mine in Longyong coalfield,kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US> kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Fujiankerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US> Provincekerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US> and Its Evolutionary Characteristicskerning: 0pt" lang=EN-US>

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kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Depositional Environment of the Tongziyan Formationkerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US> kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>of Dinfengshan Coal Mine in Longyong coalfield,kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’" lang=EN-US> kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Fujiankerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US> Provincekerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US> and Its Evolutionary Characteristicskerning: 0pt" lang=EN-US>

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kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>The Effect of the Reservoir Space in Carbonate Formationkerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: Verdana" lang=EN-US> kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>by Fracturekerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">:kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Taking the Ordovician Carbonate Formation kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>in Lungudong Region of Tarim Basin as an Example

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kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>The Effect of the Reservoir Space in Carbonate Formationkerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: Verdana" lang=EN-US> kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>by Fracturekerning: 0pt; mso-bidi-font-weight: bold; mso-ascii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">:kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>Taking the Ordovician Carbonate Formation kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>in Lungudong Region of Tarim Basin as an Example

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