- Article
20 Pages
Regional classification of dominant discontinuity sets supports open-pit slope characterization, but dip direction is circular and should not be analyzed as a linear variable. We reanalyzed 73 area-level records from 72 nominal survey areas at the Dabaoshan Open-Pit Mine; Area 9 contained two subareas. Dip direction was encoded by jointly scaled cosine and sine components, and three linear descriptors were standardized. Candidate solutions for K = 2–10 were evaluated using internal validity indices, minimum cluster size, and 300 bootstrap refits. The gap one standard error rule favored K = 2. K = 5 was retained as an exploratory engineering resolution because it had the best silhouette coefficient (0.283) and lowest Davies–Bouldin index (1.154) among K = 2–7 while retaining at least five records per cluster. Its Calinski–Harabasz index was 21.844, and bootstrap stability was moderate (adjusted Rand index, ARI = 0.643 ± 0.168). Circular mean directions ranged from 80.3° to 244.1°, with significant separation in 20,000 permutations (p < 5 × 10−5). A five-unit radial basis function (RBF) network reproduced the K-Means pseudo-labels with 97.7% ± 3.8% repeated cross-validation fidelity. This measures partition reproducibility, not independent predictive accuracy. The workflow supports structural domain screening; site-specific stability decisions require geometric, hydrogeological, and kinematic evidence.
Mining
6 October 2026



![Location of the KCMB in the southeastern part of the UDMA [34] (a), the location of the Pariz study area within the KCMB [34,82] (b), and the geological map of the Pariz study area that shows the main lithological units, faults, and known porphyry copper occurrences (c).](https://mdpi-res.com/cdn-cgi/image/width=281%2Cheight=192/https://mdpi-res.com/mining/mining-06-00091/article_deploy/html/images/mining-06-00091-g001-550.jpg)

![Schematic alteration zonation of the Roșia Poieni porphyry system (not to scale; qualitative): a potassic core (biotite, K-feldspar, quartz, chlorite, anhydrite; chalcopyrite–pyrite–minor bornite) around the Fundoaia microdiorite intrusion, overprinted by a phyllic zone (quartz, phengite, illite; pyrite-dominant, texturally abundant) and by a later, spatially irregular advanced-argillic assemblage (alunite, kaolinite, pyrophyllite), within Middle Miocene andesitic country rock. Redrawn as an original schematic from the zonation described in Milu et al. [9]; this diagram is not a reproduction of any previously published map and does not depict true areal extent or geometry.](https://mdpi-res.com/cdn-cgi/image/width=281%2Cheight=192/https://mdpi-res.com/mining/mining-06-00089/article_deploy/html/images/mining-06-00089-g001-550.jpg)

