Results 11 to 20 of about 62 (54)
Tiantangshan Rb-Sn polymetallic deposit in Guangdong Province is located at the intersection of the southern part of the NNE trending Wuyishan polymetallic metallogenic belt and the eastern end of the Nanling latitudinal polymetallic metallogenic belt ...
Tiesheng Liu +5 more
doaj +1 more source
Geochronology of the Baishi W-Cu Deposit in Jiangxi Province and Its Geological Significance [PDF]
The Baishi W-Cu deposit is located in the Nanling metallogenic belt, which is famous for its numerous W deposits and reserves. The formation age of this deposit remains unclear.
Guo-Guang Wang +3 more
core +1 more source
Abstract The current study aims at assessing the capabilities of five machine learning models in terms of mapping tungsten polymetallic prospectivity in the Gannan region, China. The five models include logistic regression (LR), support vector machine (SVM), random forest, convolutional neural network (CNN), and light gradient boosting machine (LGBM ...
Yonghang Lou, Yue Liu
wiley +1 more source
Abstract By harmonically fitting the arrival times of the P‐to‐S converted phases from the Moho, we systematically investigate the crustal anisotropy beneath the Cathaysia Block (CaB) and the surrounding areas in South China for the first time. The measured anisotropy parameters show strong lateral variations with an average splitting time of 0.35 ± 0 ...
Mengkui Li +3 more
wiley +1 more source
Geochronology and Geochemistry of the Xianghualing Granitic Rocks: Insights into Multi-Stage Sn-Polymetallic Mineralization in South China [PDF]
Multi-stage magmatic events associated with large tungsten-tin polymetallic deposits in the Nanling Range have been the subject of extensive research spanning many years.
Huan Li +5 more
core +1 more source
The tungsten deposits in NE China can be divided into four mineralization periods, namely 300–290 Ma, 250–230 Ma, 200–180 Ma, 150–130 Ma. The granites of Shamai deposit could have originated by partial melting of the juvenile crust mixed with mantle‐derived components. Mixing of various fluids are the main mechanism of mineralization in Shamai deposit.
Qingsong Dong +5 more
wiley +1 more source
Abstract Deep autoencoder (AE) networks show a powerful ability for geochemical anomaly identification. Because of little contribution to the AE network, small probability samples (again, please check this) having comparatively high reconstructed errors can be recognized by the trained model as anomalous samples. However, different autoencoder networks
Bin Feng +3 more
wiley +1 more source
3D Numerical Simulation-Based Targeting of Skarn Type Mineralization within the Xuancheng-Magushan Orefield, Middle-Lower Yangtze Metallogenic Belt, China [PDF]
Recent exploration has identified a series of Cu-Mo skarn deposits within the Xuancheng-Magushan orefield. The orefield forms part of the Nanling-Xuancheng mining district, which is located within the Middle-Lower Yangtze River Metallogenic Belt (MLYRMB)
Dai, Wenqiang +8 more
core +1 more source
Composition of Garnet from the Xianghualing Skarn Sn Deposit, South China: Its Petrogenetic Significance and Exploration Potential [PDF]
The Xianghualing skarn Sn deposit in the southwestern part of the southern Hunan Metallogenic Belt is a large Sn deposit in the Nanling area. In this paper, the garnet has been analyzed by laser ablation-inductively coupled plasma-mass spectrometry (LA ...
Qihai Shu +7 more
core +1 more source
In situ Raman spectra of aqueous K2WO4‐HCl, K2WO4‐HCl‐NaCl, and K2WO4‐CO2‐NaCl solutions were collected at elevated temperature (T, 100–400°C) and constant pressure (P) of 30 MPa. The stretching vibration band of the W=O bond (v1) was analyzed to reveal the species of tungsten (W) responsible for the hydrothermal transport of W during mineralization ...
Xiaolin Wang +6 more
wiley +1 more source

