• 责任者：Wei Xiangfeng (Institute of Resources and Environment ; Southwest Petroleum University ; Chengdu 610500 ; Sichuan China) ; Zhang Tingshan
• 刊名：Geology in China
• 出版年：2009
• 卷期：36(2)
• 关键词：沉积相 ; sedimentary facies ; 贵州 ; Guizhou Province
• 页码：p.334-343
• 图表：8 illus., 1 table, 20 refs.
• 分类号：0803
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan" class=MsoNormal>mso-font-kerning: 0pt" lang=EN-US>mes New Roman">The depositional facies of Lower Triassic Jialingjiang Formation in Chishui area of ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />me w:st="on">Guizhoume> Province belongs to continental-marine carbonate platform deposition. Based on field outcrop in combination with drill core, this paper divided the sedimentary facies into several types and pointed out that beach subfacies and dolomite-flat microfacies are depositional facies zones in favor of the development of T₁j^2-1-T₁j¹ and T₁j^5-1 reservoirs in this area and, using the “single factor analysis and multifactor integration graphing method”, obtained compositional thickness percentage distribution trend of different petrographic categories in the T₁j^2-1  layer. On such a basis, the depositional facies of T₁j^2-1-T₁j¹ and T₁j^5-1 favorable segments were also analyzed. ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />