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FENG Weiming, LI Rong, ZHAO Zhan, YU Qian, YANG Han, XIE Yuan, YE Dingnan. Boundary definition of Wufeng Formation and Longmaxi Formation in well DD1 and sedimentary environment evolution of Northeastern Yunnan[J]. GEOLOGY IN CHINA, 2021, 48(1): 297-308. DOI: 10.12029/gc20210120
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Although the Upper Ordovician Linxiang Formation marl in DD1 well is covered with thick silty mudstone, there is a lack of graptolite fossil, and no Hirnantia limestone marker stratum of the Guanyinqiao Member. Therefore, it is difficult to determine the boundary between Ordovician System and Silurian System by biostratigraphic and petrostratigraphic methods. The analysis of trace elements and REE of silty mudstone in the well DD1 shows that Th, Sr, Y, Th/U, Cen, Eun, δCe and δEu curves at the middle part of silty mudstone (1288.3m) present sharp abnormal peaks with significantly higher ΣREE content of silty mudstone (1288.3m) than its upper and lower silty mudstone and great right slope of the REE distribution curve. By comparing the elemental geochemistry characteristics of the well DD1 with other O-S boundary in the Yangtze Region, it can be concluded that there exists Guanyinqiao Member of Wufeng Formation in the well DD1, and the thickness of this marker layer is also less than 1 m. The geochemical redox discriminant graph shows that the sedimentary water medium mainly was in weak oxidation environment from the Wufeng period to the early Longmaxi period, and its oxidation was the strongest in the Guanyinqiao period. According to the analysis of sedimentary markers, the evolution process of the sedimentary facies at the O-S transition is as follows:subtidal → intertidal → supertidal → intertidal; in the Guanyinqiao period, the water was the shallowest, and there existed supertidal deposits.
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汤聪，符力耘，肖富森，杜启振. 金属矿地震勘探进展与展望. 地球与行星物理论评. 2022(02): 187-203 .
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李天成，方维萱，王磊，陈家乐，张平. 综合地球物理方法找矿应用：以智利科皮亚波地区月亮山磁铁矿型IOCG矿床为例. 地质力学学报. 2022(01): 22-35 .
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孟贵祥，邓震，祁光，汤贺军，肖艳东，王召林，薛融晖. 新疆东准噶尔成矿带浅覆盖区地质填图效果——以杜热一带浅覆盖区基岩地质填图为例. 地质通报. 2022(Z1): 374-387 .
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徐波，黄旭，蔡晓兵，王克友. 长江中下游安徽段离子吸附型稀土矿成矿条件分析. 四川地质学报. 2021(02): 209-214 .
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吕庆田，孟贵祥，严加永，张昆，龚雪婧，高凤霞. 长江中下游成矿带铁-铜成矿系统结构的地球物理探测:综合分析. 地学前缘. 2020(02): 232-253 .
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李轲，陈鹏，何宗南. 长江中下游成矿带的地质构造演化研究. 世界有色金属. 2020(06): 241-242 .
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吴迪，于炳松，吴才来，雷敏，徐楠，郑坤. 安徽铜陵焦冲矿田侵入岩锆石U-Pb定年、Hf同位素特征及成因. 中国地质. 2020(04): 1069-1091 .
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陈昌昕，严加永，周文月，王志辉，张代磊. 地热地球物理勘探现状与展望. 地球物理学进展. 2020(04): 1223-1231 .
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郑洪伟，李廷栋，贺日政. 长江中下游成矿带深部结构层析成像图像揭示华北板块的东南向俯冲. 地球科学. 2020(11): 4187-4197 .
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WAN Qiu，DU Jianguo，YANG Bo，LAN Xueyi，XIAO Xiao，SHI Ke. Deep Mineralization Background and Metallogenic Regularity of the Tongling Ore District. Acta Geologica Sinica(English Edition). 2020(06): 1893-1908 .
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汪青松，张顺林，张金会，张家嘉，尤淼. 皖东北厚覆盖区构造蚀变岩型金矿勘查模式与关键技术——以五河金矿整装勘查区为例. 安徽地质. 2020(04): 295-301 .
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陈宣华，邵兆刚，熊小松，高锐，刘雪军，王财富，李冰，王增振，张义平. 祁连造山带断裂构造体系、深部结构与构造演化. 中国地质. 2019(05): 995-1020 .
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