In order to make the distribution of lateral physical properties and layer parameters between adjacent measuring points smoother and more continuous and reduce the limitations of a single geophysical inversion method，a pseudo-two-dimensional lateral constrained joint inversion study of controlled source audio frequency magnetotelluric method (CSAMT) and micro-motion spectrum ratio method was carried out. The microtremor data is numerically simulated using the spectral ratio method，combined with the CSAMT-based limited memory BFGS (L-BFGS) inversion algorithm，introducing the lateral constraint theory，and adding the cross-gradient function to achieve the mutual coupling of two different physical parameters. A set of quasi-two-dimensional lateral constraint joint inversion algorithms was developed，and the accuracy and effectiveness of the algorithms were verified through two sets of theoretical models. Meanwhile，the inversion algorithm is used to invert the measured data in Yanqing，Beijing. The results show that there is a good correspondence between the abrupt interface morphology of resistivity and shear wave velocity，which proves the practical value of the laterally constrained joint inversion algorithm.

High-quality field seismic data are fundamental to the refined processing of seismic signals and the accurate interpretation of geological information. A scientifically designed observation system is essential to ensure data quality and imaging effectiveness. In complex geological settings，traditional acquisition systems are prone to insufficient energy coverage and imaging shadow zones，which hinder the identification of reflection signals and the detailed delineation of target structures. To enhance seismic imaging performance under such conditions，this study conducts a systematic investigation into acquisition parameter optimization for observation systems in structurally complex areas，based on an illumination analysis approach using the one-way wave equation. Forward illumination analysis is first employed to optimize the layout of sources and receivers, thereby improving energy coverage over target horizons. Subsequently，reverse illumination analysis is used to refine shot point densification，receiver array length，and channel spacing，aiming to enhance energy acquisition and wavefield coverage. A two-dimensional geological model is constructed，and forward modeling is performed to quantitatively compare the illumination energy distribution before and after optimization，leading to the determination of acquisition parameters that meet imaging requirements. Results show that the optimized observation system effectively reduces imaging shadows in complex structural zones，improves profile continuity and reflection energy response，and exhibits strong adaptability and engineering feasibility. The proposed optimization workflow has been applied and validated in an actual survey area，demonstrating consistent improvements in imaging performance. This work confirmed the practical value of illumination-based analysis in the acquisition design for complex geological conditions and established a parameter configuration methodology suitable for fault-intensive zones and sand body development areas，which will provide a replicable design reference and technical path for future seismic exploration.

Dalishu uranium deposit is a carbonate rock type uranium deposit located at the Lukan fault hanging wall in the southeast limb of Xiongwu anticline. Researches on this uranium deposits are still seldom reported. Based on the field geological survey and collection of uranium ore samples in trenches and boreholes, this paper conducted a study on mineralogy，geochemistry，and genesis of the deposit. The study show that the ore body is controlled by the northeast-trending faults and the secondary Si-Ca structural planes and closely related to organic matters. The main uranium minerals in the ore are pitchblende and uraninite，and the uraninite minerals,which are closely associated with pyrite and “black”organic matters. The trace elements such as V，Cr，Co，Ni，Cu，Zn，and Mo are enriched in the ore and the wall rocks.The rare earth element distribution pattern is“right-inclined” with the enrichment of LREE and negative δEu anomaly，indicating a certain genetic relationship with the Cambrian black rock series. It believed that the ore-forming materials maybe come from the Cambrian Niutitang and Laoba formation，the deposit was formed by deep hydrothermal action which extracted the uranium from the Cambrian basement ore-forming materials and carried to favorable areas under the orogenic background of Himalayan period.

To address the applicability challenges of geophysical water exploration methods in the Carboniferous Huangjin formation of carbonaceous-argillaceous limestone characterized by uneven development of dissolution fissure，complex hydraulic connectivity of argillaceous shale interlayers，concealed groundwater occurrence conditions，scant water resources，and improve the success rate of water well drilling, This paper adopts high-density resistivity and Audio-frequency Magnetotelluric Sounding (AMT) methods to detect low-resistivity anomalies in an area of Shaoshui town，Guilin. By applying the induced polarization (IP) secondary time difference method to analyze and delineate water-induced anomalies within these low-resistivity zones. the spatial distribution and occurrence characteristics of groundwater were identified. Results indicate that the AB/2 positions characterized by low-resistivity anomalies，positive induced polarization secondary time difference values with good continuity correspond to the actual aquifer locations. Meanwhile，areas with single-point values or values below 50 ms and poor continuity exhibit low water-bearing capacity.

The southern section of Zone No. 9 in Mianhuakeng deposit is located in the middle of the Zhuguang pluton,which is a rich in uranium. The fault zone has undergone multiple tectonic and hydrothermal action ，forming the favorable space for uranium mineralization and storage. Through secondary development and utilization of data from previous exploration projects，this paper analyzes the change patterns of the ore bodies at different elevations in the southern section of Zone 9 by the statistics on grade and thickness. The results indicate that the ore body trend to be rich in the depth but remain stable in thickness on the whole with local widening. The occurring frequency of moderate and high-grade ore segments are increasing in the deep, which may be caused by the reduction environment in the deep. This understanding provides clues and basis for the next uranium predicting and prospecting.

Zoujiashan uranium deposit is located in the west of Xiangshan ore field ，which is the biggest volcanic-type uranium ore deposits in China. The exploration in recent years have found some uranium ore bodies. Based on the finished achievement of the research and exploration practice, this papers summarized the location of uranium ore bodies in Zoujiashan as the 6 positions：1）fractures zones in main fault；2）steep parts created by volcanic collapse structures；3）the junction of faults；4）secondary fracture zone in the side of main fault；5）clamping parts of parallel faults；6）the junction of volcanic collapse structures，faults，interface of different rock. We proposed three favorable location for the future exploration, they are the stable fissure-dense sector of zone 2 in hanging the wall of F₆ main faults，the secondary fissure sector of Zone 1 beside the F₂ fault，and a “waterfall”-like interface between different rock strata in zone 4. The first and second sector should preliminary explore shallow；the third one may explore -250 m elevation or deeper. The proposed sector provide not ideas for exploring uranium deposit in Zoujiashan area，but also the resource for the mining enterprises.

Microwave plasma torch（MPT）is a new type of plasma excitation source developed by domestic research team. It is a soft ionization technology with atmospheric ionization characteristics and is mostly used for the analysis of organic matter. Compared with inductively coupled plasma（ICP）ionization sources，MPT has low ionization energy and is difficult to ionize the tested elements into metal ions，which limits its application in inorganic detection. In order to broaden the application range of MPT source，linear ion trap mass spectrometry（LTQ-MS）was used to establish a quantitative analysis method for zirconium，which was applied to environmental monitoring. The zirconium solution was introduced into the MPT-LTQ-MS experimental device，and the aerosol was produced by pneumatic atomization. After drying by concentrated sulfuric acid，the dried aerosol formed anions in the plasma flame generated by the microwave plasma moment，and was detected by LTQ-MS in the negative ion mode. The experimental results show that part of the excited zirconium ion can basically be confirmed to exist in the form of [ZrO(NO₃)₃]^-. This composite anion can be used as the characteristic signal to detect zirconium in water samples，and can be quantitatively analyzed by the characteristic spectral peak of multi-stage mass spectrometry. The characteristic signal of m/z 292 （⁹⁰Zr）showed a good linear correlation with the concentration of zirconium in the concentration range of 5~100 μg·L^-1(R²=0.998 8). The limit of detection (LOD) of the method was 2.6 μg·L^-1，and the precision (RSD) was better than 8.9 %. The content of zirconia in surface water was determined by MPT-LTQ-MS，ranging from 0.34 to 3.22 μg·L^-1，and the recovery of standard addition was 94 % to 105 %. The results show that MPT-LTQ-MS can be used as a simple method for the determination of zirconium，and can be used in environmental monitoring and drinking water testing.

The Ordos basin is the second largest energy basins in China，and several large uranium ore deposits have been discovered. The upper member of Lower Cretaceous Huanhe formation in the basin is the main prospecting horizon. In this paper，the uranium mineralization characteristics and metallogenic mechanism of Lower Cretaceous Huanhe formation in northern Ordos basin are studied by means of geological characteristics，altered mineral association，rock geochemistry and the metallogenic model is established. The three superimposed system domains of Lower Cretaceous Huanhe formation formed a fine-coarse-fine stratigraphic structure，which provided a foundation for the migration of uranium ore-forming fluids in the later period. In the early stage of mineralization，the scale of the oxidation zone was limited，and the main alteration minerals were hematite，limonite，pyrite，chalcopyrite，sphalerite，calcite and coffinite，etc. The metallogenic environment were of strong reducing capacity，the ore-forming fluid were strongly alkaline，and intense water-rock interaction occured. In the middle and late stage of mineralization，the oxidation zone advanced into the basin，a strong REDOX reaction developed ，the primary ore zone and reduction zone were formed，and the metallogenic environment maintained the early strong reducibility. The main altered minerals in this period were hematite，limonite，pyrite，montmorillonite，chlorite and uranite. With the mixing of ore-forming fluids，ore-forming fluids gradually turn to weak alkaline，uranyl silicate ions decomposed，and a large amount of uranite was formed.

In seismic exploration，high-resolution seismic reflection imaging data volumes are critical tools for achieving fine identification of thin sandstone bodies and fault structures in sedimentary basins. However，actual seismic imaging profiles often face the loss of low- and high-frequency signals，leading to low seismic imaging resolution and ineffective identification of oil，gas，uranium，coal，and other mineral resources. In signal processing，integral and differential algorithms of effective signals respectively reflect their low- and high-frequency components. Based on this principle，this paper proposes an interpretative high-resolution processing method using multi-level fractional calculus. By separately calculating different fractional-order components of effective signals，the missing low- and high-frequency components in seismic imaging profiles are obtained. Through the introduction of multivariate Gaussian theory，Bayesian theory，and statistical inversion to improve the solving process of weighting coefficients，a broadband high-resolution seismic imaging profile is established. Compared with traditional calculus-based high-resolution processing methods，this method effectively enhances the accuracy of weighting coefficient determination and avoids the impact of calculation errors on precision. Processing results from both onshore and offshore actual data demonstrate that the proposed method significantly improves the resolution and frequency bandwidth of seismic data，thereby enhancing high-resolution identification of sand bodies and related structures.

Under the background of developing digital economy，the digital transformation of uranium exploration is facing structural imbalances，manifested as core contradictions such as the difficulty in integrating multi-source data，technology fragmentation，and the disconnection between data flow and business flow. This paper focused on the application requirements of digital exploration technology，proposes an information architecture model of “business logic reconstruction-data asset governance-technology middle platform empowerment”as a trinity，and designed the overall blueprint of the “54321 Project”，covering five types of application systems，four supporting systems，three platforms，two types of centers and one full-process data chain, so as to solve the problem of the broken chain of“data-knowledge-decision”. The closed-loop optimization of business flow，data flow and decision-making flow was achieved through a four-dimensional collaborative architecture system. Through the data middle platform and cloud platform，the management domain and the production domain are deeply coupled. A technical support system centered on the integration and application of multi-source data is constructed，forming an integrated data ecosystem of “mining-storage-treatment-utilization”，providing a replicable theoretical framework and practical paradigm for the digital transformation of uranium ore exploration.