张淑霞^1,2,,
邹长春^1,2,,,
彭诚^1,2,
赵金环^1,2,
李宁^1,2,
张小环^1,2,
马火林³,
牛一雄⁴
1. 中国地质大学(北京)地下信息探测技术与仪器教育部重点实验室, 北京 100083
2. 中国地质大学(北京)地球物理与信息技术学院, 北京 100083
3. 中国地质大学(武汉)地球物理与空间信息学院, 北京 430074
4. 中国地质调查局发展研究中心, 北京 100037

基金项目: 中国地质调查局地质调查专项（12120113017600），国家自然科学基金委重大项目（41790455），中国地质调查局公益性基础地质调查项目（DD20179362）资助


详细信息

作者简介: 张淑霞, 女, 1991年生, 博士研究生, 地球探测与信息技术专业.E-mail:Sunny@cugb.edu.cn

通讯作者: 邹长春, 男, 1969年生, 教授, 博士生导师, 主要从事岩石物理、测井与井中物探、油气勘探和科学钻探等领域的教学和科研工作.E-mail:zoucc@cugb.edu.cn

中图分类号: P631

收稿日期:2017-04-09
修回日期:2018-07-14
上线日期:2018-11-05

Abnormally high natural radioactivity zones in the main borehole of the Continental Scientific Drilling Project of Cretaceous Songliao Basin: Geophysical log responses and genesis analysis

ZHANG ShuXia^1,2,,
ZOU ChangChun^1,2,,,
PENG Cheng^1,2,
ZHAO JinHuan^1,2,
Li Ning^1,2,
ZHANG XiaoHuan^1,2,
MA HuoLin³,
Niu YiXiong⁴
1. Key Laboratory of Geo-detection(China University of Geosciences, Beijing), Ministry of Education, Beijing 100083, China
2. School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
3. Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China
4. Development and Research Center, China Geological Survey, Beijing 100037, China


More Information

Corresponding author: ZOU ChangChun,E-mail:zoucc@cugb.edu.cn

MSC: P631

--> Received Date: 09 April 2017
Revised Date: 14 July 2018
Available Online: 05 November 2018


摘要
摘要:松科2井东孔是松辽盆地科学钻探工程的主体钻孔，按照计划在全井段进行地球物理测井资料采集，为深部资源勘探及白垩纪古气候、古环境研究提供准确和全面的地球物理信息.在诸多测井方法中，自然伽马测井和自然伽马能谱测井能够测量地层的天然放射性强度和铀、钍、钾元素含量等参数，被有效地应用于放射性矿床勘查，尤其是铀资源的勘查与研究；电阻率、声波、密度和中子测井等常规测井和核磁共振成像、电阻率成像、元素俘获谱测井等特殊测井能够获取地层岩性和物性参数等信息，为铀矿勘查提供有力支持.本文利用松科2井东孔自然伽马测井资料来识别高放射性异常层；基于常规测井与特殊测井资料，结合前人的地质研究成果，分析放射性异常层的特征和成因.核测井曲线指示营城组存在两段高放射性异常层，深度分别为3096.8~3102.8 m（Ⅰ号层）、3168.3~3170.9 m（Ⅱ号层）.Ⅰ号层自然伽马值最高达360 API，铀含量范围20.5~29.3 ppm，综合测井和岩心资料判断该层为砾岩，具有铀成矿潜力；分析表明，构造条件和后生改造作用是影响Ⅰ号层铀富集的关键因素，推测断裂-火山活动和盆地抬升剥蚀为含铀地下水及油气运移至Ⅰ号层提供了通道，油气的后生还原作用最终导致了Ⅰ号异常层的铀富集.Ⅱ号层自然伽马值最高达250API，钍含量22.4~37.3 ppm，铀含量5.9~11.0 ppm，为集块熔岩及凝灰岩，高放射性异常可能是高钍含量的流纹质成分和粘土矿物对铀的吸附作用导致的.松科2井东孔营城组高放射性异常层具有埋藏深度深、铀含量高等特点，表明松辽盆地深部具有找铀矿前景.
关键词: 松辽盆地/
松科2井东孔/
高放射性异常层/
测井响应/
成因

Abstract:SK-2 East Borehole (SK-2e) is the main borehole of Continental Scientific Drilling Project of Cretaceous Songliao Basin, which is designed to acquire the geophysical log data in the whole borehole, to provide accurate, comprehensive geophysical information for resource exploration and research on paleoclimate and paleoenvironment. Among various well logging methods, natural gamma-ray logging and natural gamma-ray spectral logging can measure natural gamma-ray intensity and uranium (U), thorium (Th), potassium (K) contents, and are effectively applied to radioactive deposit exploration, especially to uranium exploration and research. Conventional logging (including resistivity, acoustic, density and neutron logging) and special logging (including nuclear magnetic resonance, resistivity imaging and elemental capture spectroscopy logging) can obtain lithologic and physical parameters of strata, offering strong support for uranium exploration. In this study, the natural gamma-ray log data was used to identify abnormally high natural radioactivity zones. Based on conventional log data, special log data and previous geological research achievements, the characteristics and genesis of radioactive abnormality were analyzed. The results show that two abnormally high natural radioactivity zones are located in deep-seated Yingcheng Formation. And their depths are 3096.8~3102.8m (Layer Ⅰ) and 3168.3~3170.9 m (Layer Ⅱ) respectively. According to the comprehensive analysis of various log data and core data, Layer Ⅰ is conglomerate, with the maximum gamma of 360 API and high uranium content (20.5~29.3 ppm). Therefore, Layer Ⅰ has uranium mineralization potential. Analysis shows that tectonic conditions and epigenetic alteration are probably the key factors affecting uranium enrichment which causes abnormally high gamma-ray intensity. It was speculated that fault movements, volcanic activity, and the basin's uplift and erosion provide uranium-bearing groundwater, oil and gas with the migration channel to Ⅰ layer. The epigenetic reduction of oil and gas eventually leads to uranium enrichment of Layer Ⅰ. Layer Ⅱ consists of agglomerate lava and tuff, with the maximum gamma of 250 API, high thorium content (22.4~37.3 ppm) and high uranium content (5.9~11.0 ppm). The rhyolitic components of high thorium content and uranium adsorption by clay minerals may cause the abnormally high gamma-ray intensity in Layer Ⅱ. The abnormally high radioactivity zones of Yingcheng Formation in SK-2e are characterized by deep burial depths and high uranium contents, indicating uranium prospecting potential in deep zones of Songliao Basin.
Key words:Songliao Basin/
SK-2 East Borehole/
Abnormally high natural radioactivity zones/
Log responses/
Genesis



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