| 何中波,冀华丽,胡宝群,卫三元,林效宾.汤原断陷古近系宝泉岭组沉积特征及其对铀成矿作用的制约[J].矿产勘查,2023,14(3):432-447 |
| 汤原断陷古近系宝泉岭组沉积特征及其对铀成矿作用的制约 |
| Sedimentary characteristics of Paleogene Baoquanling Formation in Tangyuan fault depression and its constraints on uranium mineralization |
| 投稿时间：2022-06-18 |
| DOI：10.20008/j.kckc.202303009 |
| 中文关键词: 宝泉岭组 沉积相 扇三角洲 汤原断陷 |
| 英文关键词: Baoquanling Formation sedimentary facies fan delta Tangyuan fault depression |
| 基金项目:本文受中国核工业地质局铀矿勘查项目(202006-4)和四代勘查技术项目(SD01-03)联合资助。 |
| 作者 | 单位 | | 何中波 | 东华理工大学 地球科学学院, 江西 南昌 330013
核工业北京地质研究院, 北京 100029
中核集团铀资源勘查与评价技术重点实验室, 北京 100029 | | 冀华丽 | 核工业北京地质研究院, 北京 100029
中核集团铀资源勘查与评价技术重点实验室, 北京 100029 | | 胡宝群 | 东华理工大学 地球科学学院, 江西 南昌 330013 | | 卫三元 | 核工业北京地质研究院, 北京 100029
中核集团铀资源勘查与评价技术重点实验室, 北京 100029 | | 林效宾 | 核工业北京地质研究院, 北京 100029
中核集团铀资源勘查与评价技术重点实验室, 北京 100029 |
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| 中文摘要: |
| 本文以汤原断陷古近系宝泉岭组为主要研究目标层位,开展了沉积岩石学特征、古沉积环境特征、沉积体系特征及层间氧化带发育特征等方面的研究,探讨了宝泉岭组发育特征及其对铀成矿作用的制约。研究认为:(1)宝泉岭组砂岩类型主要为长石岩屑杂砂岩和岩屑砂岩,岩石具典型的低成分成熟度、低结构成熟度特征,具有近物源搬运的特征；(2)古近系宝泉岭组沉积时期为陆相淡水环境,古气候表现为温湿—干热气候,地球化学环境表现为还原环境,具较高的还原容量,有利于铀元素的还原沉淀；(3)宝泉岭组发育扇三角洲相,主要砂体表现为分流河道和水下分流河道两类,其中分流河道砂体应作为研究区下一步砂岩型铀矿找矿的主攻砂体类型。 |
| 英文摘要: |
| In the paper, sedimentary petrological characteristics, paleosedimentary environment characteristics, sedimentary system characteristics, and interlayer oxidation zone development characteristics of the Paleogene Baoquanling Formation have been studied, the developmental characteristics of the Baoquanling Formation and its constraints on uranium mineralization have been discussed. Research suggests that:(1)The sandstone types of the Baoquanling Formation are mainly feldspathic lithic greywacke and lithic sandstone. The rocks have typical characteristics of low compositional maturity and low structural maturity, and are characterized by near source transport; (2) The Paleogene Baoquanling Formation was deposited in a continental freshwater environment, with a paleoclimate characterized by a warm humid dry hot climate, and a geochemical environment characterized by a reduction environment with high reduction capacity, which is conducive to the reduction and precipitation of uranium elements; (3) The Baoquanling Formation develops fan delta facies, and the main sand bodies are divided into two types:distributary channels and underwater distributary channels. The distributary channel sand bodies should be the main type of sand bodies for the next exploration of sandstone type uranium deposits in the study area. |
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