Prediction of the Location of Concealed Pluton on the Spatial Variation Characteristics of Volatile Matter in Coal Seams

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2024-06-29 DOI:10.1155/2024/9455853
Yihao Li, Jingui Zhao, Wensheng Li
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引用次数: 0

Abstract

The lower the volatile value of coal, the higher the metamorphic degree of coal. As a vector, the spatial variation of the volatilization value of the coal seam be used to explore the location of concealed pluton and to characterize the maximum influence intensity of the magma thermal field. The eastern side of the Huyanshan intrusive pluton has amassed a large amount of C-P coal measurement and coal quality exploration data. The zonation distribution of coal seam volatile fraction data within the exploration area serves as an efficacious record of the intrusion process of the rock mass and a valuable resource for the exploration of the location of concealed plutons. Based on the data from 470 boreholes in the exploration area, contour maps of coal seams No. 02, No. 2, No. 6, No. 8, and No. 9; the true thickness contour maps of each coal layer; and the volatilizing profile map were created. The results indicate the following: (1) In the central region of the exploration area, from No. 9 to No. 8 to No. 6 to No. 2 to No. 02, the contours of volatiles in each coal seam exhibit a ring pattern, with the size of the ring and the size of the volatiles change regularly. This pattern strongly suggests that the concealed pluton is developed in the underlying layer of the coal seam. (2) According to the linear fitting of the relevant data, it is predicted that the concealed pluton is located at a depth of 65.4 m below the No. 9 coal seam. At a vertical distance of 159.1 m, the thermal field influence of the concealed pluton is lost, which aligns with the spatial distribution characteristics of volatiles in the coal seam as observed through drilling. (3) The occurrence of a significant interlayer slip between coal seam No. 6 and coal seam No. 2 in the overlying concealed pluton is indicated by the results of the hotspot migration analysis. The results are helpful to the search for magmatic-hydrothermal deposits and the exploration and development of coal and coalbed methane.

Abstract Image

根据煤层中挥发性物质的空间变化特征预测隐伏岩体的位置
煤的挥发值越低,煤的变质程度越高。煤层挥发值的空间变化作为一个载体,可用于探明隐伏柱体的位置,表征岩浆热场的最大影响强度。呼延山侵入岩体东侧已积累了大量的C-P煤测量和煤质勘探数据。勘探区内煤层挥发分数据的分区分布是岩体侵入过程的有效记录,也是隐伏岩体位置勘探的宝贵资源。根据勘探区 470 个钻孔的数据,绘制了 02 号、2 号、6 号、8 号和 9 号煤层等值线图、各煤层真实厚度等值线图和挥发剖面图。结果表明(1)在勘探区中部,从 9 号到 8 号到 6 号到 2 号到 02 号,各煤层的挥发物等值线呈现环状,环的大小和挥发物的大小有规律地变化。这一规律有力地说明了隐伏岩体发育在煤层的底层。(2)根据相关数据的线性拟合,预测隐伏岩体位于 9 号煤层下 65.4 米深处。在垂直距离159.1米处,隐伏岩体的热场影响消失,这与钻探观测到的煤层中挥发物的空间分布特征相吻合。(3)热点迁移分析结果表明,上覆隐伏岩体 6 号煤层与 2 号煤层之间存在明显的层间滑移。这些结果有助于寻找岩浆-热液矿床以及煤炭和煤层气的勘探和开发。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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