Characterization of Ore‐Forming Fluids in the Lanuoma Sediment‐Hosted Pb‐Zn Deposit, Sanjiang Tethys Region, Southwestern China: Evidences From Fluid Inclusions, Rare Earth Elements, and C‐O‐Sr‐Nd Isotopes

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ABSTRACTThe Lanuoma deposit, situated in the Changdu Basin of Southwestern China, is a unique sediment‐hosted Pb‐Zn‐Sb deposit. Three hydrothermal stages are present: (1) premineral stage, oolitic pyrite + calcite + gypsum + barite; (2) syn‐mineral stage, further divided into (2a) early stage, with the main Zn‐Pb‐Sb precipitation (sphalerite + robinsonite + galena + calcite); (2b) late stage (orpiment + realgar + calcite + minor sulfides); and (3) postmineral stage, coarse‐grained calcite. The calcites of Stage 2a are characterized by lower ΣREE concentrations (0.97–3.32 ppm) associated with positive Eu anomalies (1.13–1.98) and higher ΣREE concentrations (10.65–17.17 ppm) associated with negative Eu anomalies (0.57–0.59), indicating that the ore‐forming fluids were a mixture of two distinct fluid sources. The increasing trend of Ce anomalies (Stage 2a = 0.97, Stage 2b = 1.05, Stage 3 = 1.08) shows enhancement of fluid reducing conditions during hydrothermal evolution. The δ13CV‐PDB and δ18OV‐SMOW values also differ between Stage 2a (δ13CV‐PDB = −4.9‰ to 3.0‰; δ18OV‐SMOW = 11.4‰ to 16.6‰), Stage 2b (δ13CV‐PDB = −4.7‰ to −0.4‰; δ18OV‐SMOW = 14.2‰ to 20.4‰), and Stage 3 (δ13CV‐PDB = −4.0‰ to 1.7‰; δ18OV‐SMOW = 17.1‰ to 20.6‰), indicating a mixture of deep‐seated magmatic fluid and dissolved marine carbonate rocks. Corresponding δ18Ofluid values of the hydrothermal fluid are 2.4‰–7.0‰ in Stage 2a, 4.9‰–8.5‰ in Stage 2b, implying a combination of deep‐seated magmatic fluids and sedimentary formation water. Initial 87Sr/86Sr ratios of calcite from Stage 2a (0.7084–0.7086) fall between the values characteristic of the mantle, metamorphic basement, and Bolila Formation, implying a mixed source. Calcite in Stage 2a has higher εNd(t) values (−0.51 to −1.82) compared to Stage 2b and Stage 3 (−3.91 to −9.96). This indicates there was more input of mantle‐sourced materials during Pb‐Zn mineralization. Systematic microthermometric analysis demonstrates an isothermal mixing of two fluid sources (averaging at 189°C) with different salinities (ranging from 3.87% to 19.05% NaCl eqv; i.e., low‐salinity magmatic fluid and high‐salinity brines) during Pb‐Zn mineralization. These results suggest that the Lanuoma Pb‐Zn deposit was formed by the mixing of two distinct mineralizing fluid sources: (1) magmatic‐hydrothermal fluids derived from deep‐seated magmas, which transported reducing agents such as sulfur; and (2) high‐salinity brines enriched in metals, likely leached from carbonate wall rocks and metamorphic basement.

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BackgroundVarus ankle osteoarthritis is classified using only weightbearing anteroposterior ankle radiographs; however, sagittal ankle alignment may also affect the position and extent of joint space obliteration. We hypothesized that the sagittal alignment of the ankle may also affect the position and extent of joint space obliteration visible on the coronal section; therefore, we identified the sites of joint space obliteration in patients with stage 3 varus ankle osteoarthritis for comparison with the sites observed on simulated weightbearing computed tomography and investigated the effects of anterior and posterior ankle subluxation.MethodsSimulated weightbearing computed tomography scans of 83 ft with varus ankle osteoarthritis (26 stage 3a, 57 stage 3b) were performed to check for joint space obliteration in the ankle. Further classification as exhibiting either anterior, posterior, or no subluxation on weightbearing lateral radiographs was performed.ResultsAnterior, posterior, and no subluxation was seen in 5, 9, and 12 ankles among the 26 classified as stage 3a, respectively, and in 22, 12, and 23 ankles among the 57 classified as stage 3b, respectively. The mean tibial lateral surface angle on weightbearing lateral radiographs in stage 3a ankles was 75.6, 83.3, and 80.3 degrees in the anterior, posterior, and no subluxation groups, respectively; and 75.5, 86.6, and 82.7 degrees in stage 3b ankles (p < .05). In stage 3b ankles, widespread joint space obliteration was observed at the anterior distal articular surface of the tibia in all 22 ankles with anterior subluxation and at the posterior distal articular surface of the tibia in all 12 ankles with posterior subluxation.ConclusionsSimulated weightbearing computed tomography revealed joint space obliteration at the anterior distal articular surface of the tibia in stage 3b ankles with anterior subluxation and at the posterior side in stage 3a and 3b ankles with posterior subluxation. In some patients with stage 3 varus ankle osteoarthritis, the obliteration of the joint space is difficult to evaluate accurately using only weightbearing anteroposterior radiographs; weightbearing lateral radiographs should also be performed.

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Chronic kidney disease in Taiwan – Authors' reply

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