... classification issues. Arsenmarcobaldiite was collected in a small prospect located at Verzalla (latitude 43°58′03″ N, longitude 10°16′41″ E) where baryte + pyrite lenses embedded in schists crop out. This locality is placed between the Pollone and Monte Arsiccio mines, in the Sant’Anna tectonic window...

... several thousand P- and S-wave arrivals on geophone data, while Huot et al. (2022) used a similar approach and handpicked event windows on DAS data to train a CNN. However, handpicking events is a time-consuming task and is not feasible for real-time applications. Boitz and Shapiro (2024) trained...

... Arsiccio mine; several years later, these samples were identified as Sb-rich graeserite (Biagioni et al. , 2020a ). Mario Bianchini provided several mineral samples for the investigation of the mineralogy of ore deposits located in the Sant'Anna tectonic window (in particular, the Pollone and Monte...

.... The continuous field data were divided into overlapping patches using a 1.3 m sliding window along the depth direction, with a step size of 0.325 m. To avoid data leakage, two 3.6 m continuous sections were extracted from each well, forming an independent 57.6 m test set. The remaining image patches from...

...F ig . 1. Geological map of the Sant’Anna tectonic window, showing the most important mineral deposits: the Pollone barite – pyrite – (Pb–Zn–Ag) deposit (P1 to P6 outcrops), the Cu(Au) vein system of Buca dell’Angina, and the Monte Arsiccio barite – pyrite – iron oxides deposit (modified from...

... 2 2014 The baryte-pyrite-Fe oxides deposit of Monte Arsiccio (43°58′N, 10°17′E) is located in the northeastern portion of the Sant'Anna tectonic window, an area in which outcrops of metamorphic rocks are surrounded by the non-metamorphic sedimentary formations of the overlying Tuscan Nappe...

... mineral species sulfosalt thallium lead antimony arsenic Monte Arsiccio mine Apuan Alps Tuscany Italy The barite – pyrite – iron oxides deposit of Monte Arsiccio is located in the northeastern portion of the Sant’Anna tectonic window ( Fig. 1 ). In this area, metamorphic rocks of the Apuan...

... and discussion of the crystal chemistry of the routhierite isotypic series. The baryte-pyrite-iron oxide deposit of Monte Arsiccio (latitude 43°58′N, longitude 10°17′E) is located in the northeastern portion of the Sant'Anna tectonic window, an area in which outcrops of metamorphic rocks are surrounded...

... outcrops associated with the ore deposits of Sant’Anna tectonic window and Fornovolasco ( Fig. 1a ), proposing that they are tourmaline-bearing intrusive rocks probably related to a buried pluton. The interpretation as intrusive bodies, however, was not completely accepted by following authors...

... and Prehistorical Museum ‘Don Alberto Benedetti’ (Museo Paleontologico e Preistorico) of Sant'Anna d'Alfaedo, Verona Province, Italy (MPPSA IGVR 91032) and some specimens from the Chalk Group of southern England (UK). The English material includes a disturbed tooth set with a single vertebral centrum housed...

..., longitude 10°17’E) is located in the Southern Apuan Alps and, in particular, in the northeastern sector of the Sant’Anna tectonic window. In this area, metamorphic rocks belonging to the Apuane and Fornovolasco-Panie units crop out through the non-metamorphic sedimentary formations belonging to the Tuscan...

.... (2019) Arsenmarcobaldiite, Pb 12 (As 3.2 Sb 2.8 ) Σ=6 S 21 , a new N = 3.5 jordanite homologue from the Sant'Anna tectonic window, Apuan Alps (Tuscany, Italy) . European Journal of Mineralogy 31 , 1067 – 1077 . Bindi, L., Garavelli, A., Pinto, D., Pratesi, G...

... over the station corrections. In particular, as station Sant’Anna di Valdieri houses both a 3c and a 1c sensor (code stv and stv2 for the 1c and 3c sensors, respectively), new coefficients for the M L scale from 3c recordings are computed by setting to zero the station correction...

... ). Geochemical evidence confirmed that these reservoirs were sourced by both lacustrine and marine synrift source rocks in different proportions. The migration pathways were through carrier beds and windows produced by halokinesis in the salt section. In this postsalt trend, the main seals are interbedded shales...

.... the Pollone and the Monte Arsiccio mines, are located in the Sant'Anna tectonic window, an area in which metamorphic rocks belonging to the Apuan Alps metamorphic complex are surrounded by the non-metamorphic sedimentary formations of the Tuscan Nappe. In particular, the Pollone mine, located in the southern...

... and Triassic metadolostone, in the northeastern sector of the Sant’Anna tectonic window. The Monte Arsiccio mine is the type locality for nine other mineral species, among which are some other sulfosalts: boscardinite ( Orlandi et al. 2012 ), protochabournéite ( Orlandi et al. 2013 ), arsiccioite ( Biagioni et...

... low a crystallinity for structural analysis. For details on sample preparation and characterization see Porta et al. (1991) . A crystal of malachite was picked from a specimen found in the Fontana tunnel, Argentiera di Sant'Anna mine, Apuan Alps, Italy. Malachite occurs as euhedral prismatic...

... of Verona province ( Fig. 1A , B ). The specimen, first reported by paleontologist Achille De Zigno (1883a ,b), was rapidly forgotten and re-discovered only a few decades ago. This fossil acquired historical importance over the years, as it represents an additional window to the early stages of research...

... deposits. In this paper new crystal-chemical data on chovanite are presented and its 8 Å structure is detailed according to the principles of modular analysis. The Monte Arsiccio and Pollone mines are located in the northeastern and southwestern portions of the Sant'Anna tectonic window...