首页|铀成矿与红层盆地关系再讨论——以湘赣边界鹿井铀矿田为例

铀成矿与红层盆地关系再讨论——以湘赣边界鹿井铀矿田为例

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鹿井铀矿田是我国华南地区最重要的硬岩型铀矿田之一,矿田内铀矿床围绕丰州盆地分布,红层盆地与铀成矿的关系已经讨论并争议了近40年。本文开展了铀矿带与丰州盆地红层盖层相关性研究,结合鹿井矿田隆升剥露历史和南雄盆地北缘断裂变形特点,认为丰州盆地是晚白垩世—古近纪红层盆地底部沉积的残留,是一个规模大很多的红层盆地的一小部分,其上有约1。5~2。5 km厚的红层沉积物已经被剥蚀了。铀成矿与红层盆地没有必然的成因关系,热液型铀矿床早期成矿作用发生于红层盆地形成之前,成矿后在约95~75 Ma被抬升剥露至地表;然后被红层盆地覆盖保存,至65~55 Ma被埋藏至最深(约1。5~2。5 km);约55~45 Ma再次被隆升剥露降温,至40 Ma左右已至近地表常温状态,40 Ma以来一直稳定在近地表常温状态。而遂川断裂NW侧在约15 Ma的中新世中期才开始快速隆升剥露,北西盘比南东盘隆升幅度更大,反映了遂川断裂的左行走滑特征,该断裂与热水断裂的叠接带以拉分盆地性质减缓隆升剥露幅度,才得以保存现有的丰州盆地。丰州盆地对早于盆地沉积所形成的铀矿床起到了保矿作用。因此,其找矿方向是除了丰州盆地周边以外,丰州盆地底下是铀矿找矿的非常有利区段,极大地拓宽了鹿井铀矿田的找矿空间。
Re-discussion on the temporal relation between uranium mineralization and red bed basin——Taking Lujing uranium ore field in the Hunan—Jiangxi border as an example
Lujing uranium ore field is one of the most important hard rock-hosted uranium ore fields in South China.The uranium deposits in the field are distributed around Fengzhou Basin.In this paper,a study on the correlation between the uranium ore belt and the red-bed cap rock in the Fengzhou Basin has been carried out,taking into account the uplift and denudation history of the Lujing ore field and the characteristics of the faults in the northern margin of the Nanxiong basin,it is considered that the Fengzhou basin is a remnant of the late Cretaceous—Paleogene red-bed basin and is a small part of a much larger(at least 5~10 times)red-bed basin,about 1.5~2.5 km of red layer sediments have been eroded.There is no necessary genetic relationship between uranium mineralization and red bed basin.The hydrothermal uranium deposits occurred before the formation of the red-bed basin,and were exhumed to the surface(about 95~75 Ma)and then covered by the red-bed basin,it was buried to the deepest depth(about 1.5~2.5 km)at 65~55 Ma.It began to rise again and exfoliation from 55~45 Ma,and is near the surface at about 40 Ma and stable in the normal temperature of the surface since then.The NW side of the Suichuan fault began to uplift and exfoliate rapidly in the middle Miocene about 15 Ma,and the uplift range of the NW plate is larger than that of the SE plate,which reflects the left-lateral strike-slip characteristics of the Suichuan fault,the superimposed zone of the fault and the Reshui fault can preserve the existing Fengzhou basin by pulling apart the basin to slow the uplift and exhumation.The Fengzhou basin plays an important role in the preservation of uranium deposits formed before the basin sedimentation.Therefore,in addition to the surrounding area of Fengzhou basin,there is a favorable area for uranium exploration under the basin,which greatly expands the prospecting space of Lujing uranium ore field.

uranium mineralizationFengzhou basinuplift and denudation historyore-preserving structureprospecting directionLujing uranium ore field

陈柏林

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中国地质科学院地质力学研究所,北京,100081

铀成矿 丰州盆地 隆升剥露历史 保矿构造 找矿方向 鹿井铀矿田

2025

地质论评
中国地质学会

地质论评

北大核心
影响因子:1.842
ISSN:0371-5736
年,卷(期):2025.71(1)