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spanTitleEn>

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3.<SPAN style=&quot;COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold&quot; lang=EN-US>t;Times New Roman&quot;>Quantitative Evaluation of Fracture Distribution in the Down Strike-Slip Fault Zone of Upper Shuaiba Member of Lower Cretaceous, space prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; /><st1:place w:st=&quot;on&quot;><st1:City w:st=&quot;on&quot;>Daleelst1:City>, <st1:country-region w:st=&quot;on&quot;>Omanst1:country-region>st1:place> space prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; />
4.<SPAN style=&quot;COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold&quot; lang=EN-US>t;Times New Roman&quot;>Quantitative Evaluation of Fracture Distribution in the Down Strike-Slip Fault Zone of Upper Shuaiba Member of Lower Cretaceous, space prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; /><st1:place w:st=&quot;on&quot;><st1:City w:st=&quot;on&quot;>Daleelst1:City>, <st1:country-region w:st=&quot;on&quot;>Omanst1:country-region>st1:place> space prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; />
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