鄂西南地区五峰组-龙马溪组连续沉积特征
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摘要
湘鄂西地区奥陶系五峰组—志留系龙马溪组间未发育明显的奥陶系观音桥组介壳层,且至少缺失了2个笔石带,被认为是存在湘鄂西水下隆起/高地。此次研究通过对鄂西南地区奥陶系五峰组—志留系龙马溪组沉积特征及沉积环境分析,发现五峰组—龙马溪组为连续沉积,沉积水体总体呈逐渐变深—逐渐变浅的特征;在五峰组的深水陆棚相之上,发育全球冰期背景下的赫南特期浅水陆棚相,矿物组分以石英含量最高,黏土矿物含量最低,有机碳含量较高为典型特征;其元素组分以Al2O3含量相对最低,SiO2含量相对最高为特征,岩石类型为炭质泥质粉砂岩;在五峰组—龙马溪组沉积过程中,经历了明显变冷的时期,即赫南特期的存在。鄂西南地区奥陶系五峰组—志留系龙马溪组以浅水陆棚相最为发育且岩性快速变化,相对中上扬子其他地区,沉积水体较浅,对页岩气富集造成不利影响。
According to the previous research,there was a highland/underwater uplift developed in western Hubei and Hunan area,because of the absence of shell layer of Ordovician Guanyinqiao section or at least two graptolitic biozones between Ordovician Wufeng Formation and Silurian Longmaxi Formation.Based on the detailed study of sedimentary characteristics and the evolution of sedimentary environment,it can be figured out that there was nondepositional hiatus between Ordovician Wufeng Formation and Silurian Longmaxi Formation,and the existence of Hrinantian deposition.In the depositional process of WufengLongmaxi Formations,the depth of sedimentary water was from gradually deep to shallow,and the paleoclimate experienced the significant cooling period.It was shallow shelf facies of Hrinantian under the background of global ice age,which was deposited on the Wufeng deep shelf facies,most as carbonaceous pelitic siltstone with the minerals of highest content of quartz,fewest of clay minerals,and higher of organic carbon content,and with the elemental constituent of the highest SiO2 and the least Al2 O3.The shallow shelf facies was the most developed of Wufeng-Longmaxi Formations in southwestern Hubei,with rapid changes in lithology.Compared to others in Middle-Upper Yangtze area,the shallower sedimentary water was not conducive to the shale gas enrichment.
According to the previous research,there was a highland/underwater uplift developed in western Hubei and Hunan area,because of the absence of shell layer of Ordovician Guanyinqiao section or at least two graptolitic biozones between Ordovician Wufeng Formation and Silurian Longmaxi Formation.Based on the detailed study of sedimentary characteristics and the evolution of sedimentary environment,it can be figured out that there was nondepositional hiatus between Ordovician Wufeng Formation and Silurian Longmaxi Formation,and the existence of Hrinantian deposition.In the depositional process of WufengLongmaxi Formations,the depth of sedimentary water was from gradually deep to shallow,and the paleoclimate experienced the significant cooling period.It was shallow shelf facies of Hrinantian under the background of global ice age,which was deposited on the Wufeng deep shelf facies,most as carbonaceous pelitic siltstone with the minerals of highest content of quartz,fewest of clay minerals,and higher of organic carbon content,and with the elemental constituent of the highest SiO2 and the least Al2 O3.The shallow shelf facies was the most developed of Wufeng-Longmaxi Formations in southwestern Hubei,with rapid changes in lithology.Compared to others in Middle-Upper Yangtze area,the shallower sedimentary water was not conducive to the shale gas enrichment.
引文
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