新疆吐哈盆地布尔加凸起八道湾组沉积特征浅析OA
Sedimentary Characteristics of Badaowan Formation in Buerjia Bulge of Turpan-Hami Basin,Xinjiang
布尔加凸起位于新疆吐哈盆地吐鲁番坳陷西部,含铀层位为下侏罗统八道湾组.为了填补布尔加凸起八道湾组铀成矿地质背景研究的空白,文章通过野外调查、岩心观察、粒度分析、薄片鉴定等方法,首次系统总结了八道湾组砂岩型铀矿化特征、沉积相、砂体及岩石学特征,并从铀源、构造、古气候、岩性-岩相、层间氧化带等方面分析了铀成矿条件.研究认为,布尔加凸起八道湾组为一套含煤碎屑岩沉积建造,以辫状河-辫状河三角洲相沉积为主,发育3~5层砂体,砂体规模大,连通性好,是研究区目标储铀层.岩石学特征研究表明,八道湾组砂体以中砂岩、细砂岩为主,分选性好,碎屑岩以岩屑砂岩、长石岩屑砂岩为主,岩石成熟度较低,反映研究区为离物源区较近的河流相沉积,河道水动力条件较强.通过成矿条件分析认为,蚀源区富铀岩体为盆地目的层铀成矿提供了丰富的铀源,目的层形成之后经历的抬升剥蚀→稳定沉积→抬升改造作用有利于层间氧化带的发育、铀的预富集及进一步富集叠加,古气候由温暖潮湿向炎热干旱的转变有利于储铀层位的形成和砂岩型铀矿后生改造成矿作用的进行,八道湾组辫状河—辫状河三角洲相砂体和分带明显的层间氧化带有助于形成砂岩型铀矿.因此,通过上述分析认为布尔加凸起找矿潜力大,八道湾组是重点找矿层位.
Buerjia bulge is located in western Turpan depression of Turpan-Hami Basin in Xinjiang,with the uranium rich layers Badaowan Formation of Lower Jurassic.The research focused on the geological background of uranium mineralization in Badaowan Formation,the author systematically summarized the characteristics,sedimentary facies,sand bodies,and petrological features of sandstone type uranium mineralization in Badaowan Formation for the first time through field investigation,core observation,grain size analysis,thin section identification,etc.The uranium mineralization conditions were analyzed from the aspects of uranium source,structure,paleoclimate,lithology and interlayer oxidation zone.The result suggests that Baodaowan Formation in Buerjia bulge was a set of sedimentary formation of coal-bearing clastic rock,mainly composed of braided river to braided river delta facies sedimentation,with 3-5 layers of sand bodies developed.The sand bodies are large in scale and have good connectivity,making them a favorable target uranium storage layer.The study of petrological characteristics shows that the sand bodies of Badaowan Formation are mainly composed of medium sandstone and fine sandstone,with good sorting.The detrital rocks are mainly lithic sandstone and feldspar lithic sandstone,with low rock maturity,reflecting that the study area is close to the source area and has strong hydrodynamic conditions in the river channel.Through analysis of mineralization conditions,the uranium rich rock bodies in the erosion source area were believed to provide abundant uranium sources for the formation of target uranium mineralization layer the basin.The target uranium layer then experienced the process of uplift erosion→stable sedimentation→uplift transformation which made them conducive to the development of interlayer oxidation zones,pre enrichment of uranium and further mineralization superposition.Therefore,the sandstones of braided river to braided river delta facies and clearly divided interlayer oxidation zone in Badaowan Formation is the target horizons,Buerjia bulge is the key potential area for next exploration.
郭长林
核工业二〇三研究所,陕西 西安 710086
天文与地球科学
沉积相砂体岩石学成矿条件八道湾组布尔加凸起
sedimentary faciessand bodypetrologymetallogenic conditionsBadaowan FormationBuerjia bulge
《铀矿地质》 2026 (2)
276-287,12
中国核工业地质局铀矿地质勘查项目(编号:202318-2)和中国核工业地质局铀矿战略选区项目(编号:202218-3)联合资助.
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