| 新疆莎车盆地上白垩统-古近系蒸发岩沉积及成钾前景 |
| Received:April 30, 2015 Revised:February 16, 2016 点此下载全文 |
| 引用本文：CAO YangTong,LIU ChengLin,JIAO PengCheng,ZHANG Hua,WU Kun,SUN HongWei,LÜ FengLin,SU Ye.2016.Evaporite deposition and potassium enrichment prospect from Upper Cretaceous to Paleogene in Yarkand Basin, Xinjiang[J].Mineral Deposits,35(2):300~314 |
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| Author Name | Affiliation | | CAO YangTong | School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, Shaanxi, China
MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | LIU ChengLin | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | JIAO PengCheng | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | ZHANG Hua | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | WU Kun | School of Earth Sciences and Resources, China University of Geoscience, Beijing 100083, China | | SUN HongWei | School of Earth Sciences and Resources, China University of Geoscience, Beijing 100083, China | | LÜ FengLin | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | SU Ye | No. 2 Geological Party, Hebei Coal Geological Bureau, Xingtai 054000, Hebei, China |
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| 基金项目:本文为国家"十二五"科技支撑课题(编号: 2011BAB06B06)、国家"973"计划(编号: 2011CB403007)资助成果 |
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| 中文摘要:新疆莎车盆地发育大范围的蒸发岩。蒸发岩沉积与海侵-海退密切相关,自晚白垩世-渐新世以来,莎车盆地至少有5次小规模海侵-海退旋回,除阿尔塔什组石膏岩为断续海侵期沉积外,其余基本为海退期沉积。莎车盆地主要的蒸发岩沉积层位为吐依洛克组上段及阿尔塔什组。野外调查显示,吐依洛克组石盐岩露头主要沿西昆仑山前呈长条状分布,基本呈透镜体,阿尔塔什组石膏岩露头则见于盆地大部分地区,包括西昆仑山前、南天山山前及麦盖提斜坡,横向上持续稳定。野外调查及室内分析显示,盐类矿物主要为石盐、石膏、硬石膏,少量杂卤石、钙芒硝及钾石膏。盆地中石盐岩透镜体在横向上的不连续性,可能反应了吐依洛克组沉积晚期西昆仑山前存在多个次级古盐湖凹地,在干旱条件下浓缩成盐,而次级古盐湖在演化过程中大范围巨厚石膏岩的缺失,可能与当时的海退时间极短有关。依据莎车盆地蒸发岩沉积特征、盐类矿物组合、古盐湖演化环境,推测盆地有利的成钾层位为吐依洛克组上段,在乌帕尔一带发现成钾显示,可能为有利的成钾区域;而盆地小范围、厚度不大的石盐沉积及埋藏深度大为不利的找钾因素。 |
| 中文关键词:地质学 蒸发岩 成钾前景 上白垩统 古近系 莎车盆地 |
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| Evaporite deposition and potassium enrichment prospect from Upper Cretaceous to Paleogene in Yarkand Basin, Xinjiang |
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| Abstract:A wide range of evaporite deposits have been developed since late Cretaceous-Oligocene in Yarkand Basin, Xinjiang. The deposition of evaporites had a closely relationship with transgression-regression, and there developed at least five times of small transgression-regression cycles in this period. The Aertashi Formation gypsum rocks were continuous transgression sedimentation while the other strata were essentially regression sedimentation. Evaporite sedimentary layers are mainly in the upper member of Tuilok Formation and Aertashi Formation. Field work shows that rock salt outcrops are distributed in long stripe form along the foreland of West Kunlun Mountains and are characterized by lenticular sedimentation. However, the gypsum outcrops are distributed steadily laterally in most parts of the basin such as the foreland of West Kunlun Mountains, South Tianshan Mountains and Maigaiti Slope. Laboratory analysis shows that the primary saline minerals are halite, gypsum, and anhydrite, with minor polyhalite, glauberite and syngenite. The lateral discontinuity of rock salt lens may imply that there might have existed more secondary ancient salt lake depressions in the foreland of West Kunlun Mountains in late sedimentation period of Tuilok Formation, during which materials were concentrated into salt under the condition of drought, and the lack of large scale thick gypsum rock in the evolutionary process might have been related to the very short time of regression in that period. According to the evaporite sedimentary characteristics, salt mineral assemblage and the ancient salt lake evolution environment in Yarkand Basin, the authors conclude that the favorable potassium horizon is the upper member of Tuilok Formation, and the Wupaer area is probably the favorable potash-forming place, as shown by some clues. Nevertheless, the small thin rock salt deposition and large depth are unfavorable factors. |
| keywords:geology evaporites prospect of potassium enrichment Upper Cretaceous Paleogene Yarkand Basin |
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