Hydrodynamique des systèmes minéralisés péri-granitiques : étude du gisement à W-Sn-(Cu) de Panasqueira (Portugal)

The vein and greisen Sn-W deposits are magmatic-hydrothermal systems that provide an important part of the world W production and represent an important source of Sn. The formation of these deposits involves continuum of magmatic-hydrothermal processes and implies the transfer and the focusing of a large amount of mineralizing fluids. This study aims to improve understanding of hydrodynamic and geological processes involved during the transport and the deposition of metals leading to the formation of these deposits. We have performed a complete study combining (i) field works (geological and structural studies), (ii) fluid flow reconstruction via the textural analysis of tourmaline growth bands, (iii) experimental determination of permeability changes during greisenization, and (iv) numerical modeling of peri-graniticfluid flow accounting for magmatic fluid production and dynamic permeability related to fluid-rock interactions. This methodology was applied in the case of the world-class W-Sn-(Cu) Panasqueira deposit, which represents a referencesite to study magmatic-hydrothermal processes leading to the formation of large vein and greisen deposit. Our resultsdemonstrate that the releasing and the expulsion of ore-bearing magmatic fluids triggered greisenization of the apicalpart of granite intrusion, which caused generation of porosity (~8.5%) and therefore a significant increase of permeability(from 10-20 to 10-17 m²) in massive greisen composing the granite’s roof. The development of this permeable pathwayconstitutes an important drain promoting the expulsion and the focusing of magmatic fluids produced during thecrystallization of the underlying granite. This enhancement of magmatic fluids expulsion (i) promotes significantly fluidflux and transfer of metals, and (ii) the establishment of high fluid pressure conditions, which coupled with the regionalcompressive crustal regime, triggered the opening of mineralized veins above the granite roof. Finally, this studyemphasizes that reactive hydrothermal fluids are able to generate their own pathways in initially impermeable rocks. Thisprocess represents an important mechanism to enhance fluid flow and promote the formation of large hydrothermaldeposits.Les gisements à Sn-W de type veine et greisen sont des systèmes magmatiques-hydrothermaux dont l’exploitation fournit une part importante de la production mondiale de tungstène et qui représentent également une source importante d’étain. La formation de ces gisements résulte d’un continuum de processus magmatiques et hydrothermaux et implique un transport efficace et la focalisation des fluides minéralisateurs. Cette étude vise à améliorer la compréhension des processus hydrodynamiques et géologiques impliqués lors du transport et du dépôt de métaux conduisant à la formation de ces gisements. Nous avons réalisé une étude pluridisciplinaire combinant (i) travail de terrain (étude géologique et structurale), (ii) reconstruction des paléo-circulations hydrothermales via l’analyse texturale des bandes de croissance des tourmalines, (iii) détermination expérimentale des changements de perméabilité induits par la greisenisation et (iv) modélisation numérique des écoulements péri-granitiques prenant en compte l’évolution de la perméabilité dynamique lors des interactions fluide-roche. Cette méthodologie a été appliquée au cas du gisement W-Sn-(Cu) de Panasqueira, qui constitue un site de référence pour étudier les processus magmatiques et hydrothermaux conduisant à la formation de gisements à Sn-W de classe mondiale. Les résultats obtenus démontrent que l’expulsion des fluides magmatiques minéralisés a déclenché la greisenisation des parties apicales (coupoles et apex) de l’intrusion granitique, entraînant la création de porosité (~ 8,5%) qui améliore significativement la perméabilité (de 10-20 à 10-17m²) au sein du greisen massif composant le toit de l’intrusion. Le développement de ce niveau perméable constitue un drain important favorisant l'expulsion et la focalisation des fluides magmatiques minéralisateurs exsolvés lors de la cristallisation du granite sous-jacent. Cette focalisation des décharges hydrothermales (i) améliore significativement le transport des métaux, et (ii) favorise l'établissement de conditions de pression de fluide élevées qui couplées aux contraintes régionales compressives causent l'ouverture des veines minéralisées au toit de l’intrusion. Cette étude souligne l’importance des rétrocontrôles entre perméabilité dynamique et altération hydrothermale. Ces derniers constituent des mécanismes majeurs permettant d’améliorer significativement la circulation des fluides minéralisateurs et donc la formation de gisements hydrothermaux de grandes tailles

Rôle du canal ionique TRPM4 dans les cellules dendritiques

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Deciphering fluid flow at the magmatic-hydrothermal transition: A case study from the world-class Panasqueira W–Sn–(Cu) ore deposit (Portugal)

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How greisenization could trigger the formation of large vein-and-greisen Sn-W deposits: a numerical investigation applied to the Panasqueira deposit

International audienceThe formation of large tin-tungsten (Sn-W) deposits around granitic intrusions requires the circulation of large volumes of fluids within permeable structures. Half of the world’s tungsten production originates from highly mineralized veins above granitic intrusions and from the altered part of the granite (the greisen), whose formation results from intense fluid-rock interactions. During greisenization processes, mineral reactions involve a decrease in the rock volume and thus an increase in porosity and permeability. To understand the complex fluid-rock interactions leading to the formation of large Sn-W ore deposits, we conducted numerical modeling accounting for magmatic fluid production and realistic permeability changes due to granite alteration and overpressure in the hosting rocks. The water/rock ratio is computed to constrain the rate of greisenization and therefore the porosity and permeability evolution laws. Four model results are presented: with and without fluid production exsolved from the granitic magma, and with and without dynamic reaction-enhanced permeability. The formation of greisen is reproduced, and greisen thickness reaches 200 m for the more sophisticated model. The interplay between greisenization and fluid production creates zones of overpressure above the granite that could localize the permeable structures such as the veins swarm observed at Panasqueira. Dynamic permeability promotes high fluid velocity and intense fluid-rock exchanges that could result in the formation of large ore deposits by enhancing mass transfer within and above granitic intrusions

Improving prospectivity by numerical modeling of hydrothermal processes

International audience— The formation of " hydrothermal resources " , a term including mineral and geothermal resources, is the result of thermal, hydraulic, mechanical and chemical processes. Accounting for all of them (THMC modeling) is not an easy task since a large number of variables are unknown. However, when only hydraulic and thermal processes are selected, numerical tools such as the " Rock Alteration Index " can be used to predict locations of the most probable mineralized zones. As an example, 3D numerical models of the Tighza pluton (Morocco) demonstrate that computed mineralized zones correspond to those found in the field. Using geological, petrophysical data and measured temperatures, numerical simulation of the Soultz-sous-Forêts geothermal system (France) helped to understand how fluid circulation in the shallow crust is controlled. Besides reproducing temperature profiles, the obtained numerical models were also used to predict the depth and the temperature of a previously suspected anomaly (Rittershoffen area). It turned out that this anomaly (160°C at a depth of 2500m) was confirmed at the same time by temperature measurements in a borehole. Numerical modeling of hydrothermal processes should thus be considered as a predictive tool in exploration strategies

Genetic relationship between greisenization and Sn–W mineralization in vein and greisen deposits: Insights from the Panasqueira deposit (Portugal)

The W–Sn Panasqueira ore deposit is a magmatic-hydrothermal system, which includes a high-grade quartz-vein type mineralization and a disseminated greisen-type mineralization occurring in the upper part of the Panasqueira two-mica granite. We investigated the genetic and chronological relationships between the greisenization of the Panasqueira granite and the formation of ore-bearing quartz veins by monitoring major and trace elements variations in quartz-white mica assemblages composing the two-mica granite, greisen and W–Sn-bearing quartz veins. The greisen is characterized by an overall depletion in Mg, Ti, Ca, Na, Ba, Sr, REE and enrichment in Fe, Li, Rb, Cs, Sn, W which reflect the breakdown of feldspars and fluid-rock interactions with W–Sn-bearing fluids. White-mica from greisen and mineralized quartz veins are enriched in granophile elements (F, Rb, Cs, Li, Sn, W and Zn) compared to magmatic muscovite from the two-mica granite. Trace elements contents in quartz depict trends which show the progressive enrichment in Ge and B and depletion in Al, Ti and Li from magmatic to hydrothermal quartz that emphasize the progressive evolution and cooling of the magmatic-hydrothermal system of Panasqueira. Geochemical similarities between quartz-white mica assemblages from greisen and wolframite-bearing veins suggest that greisenization and the formation of mineralized veins result from the same hydrothermal event and derived from the same source of hydrothermal fluids. Apatite from greisen and quartz vein yielded U–Pb ages of 292 ± 10 Ma and 295 ± 5 Ma respectively confirming that greisenization and the formation of mineralized veins occurred roughly at the same time. These ages also overlap with the emplacement age of the Panasqueira granite (296 ± 4 Ma), indicating a temporal link between greisenization, W–Sn mineralization and granite crystallization. Temperatures of the magmatic-hydrothermal system constrained by Ti-in quartz thermometry depicts a cooling trend from magmatic quartz of granite (700–600 °C) to hydrothermal quartz of greisen (500–400 °C) and veins (450–350 °C). These results suggest that greisenization and the formation of W–Sn bearing quartz veins occurred at the magmatic-hydrothermal transition, during which orthomagmatic fluids rich in volatils, incompatible elements and W–Sn were exsolved during the final solidification stage of the Panasqueira two-mica granite

Exploring complementarities between modelling approaches that enable upscaling from plant community functioning to ecosystem services as a way to support agroecological transition

International audiencePromoting plant diversity through crop mixtures is a mainstay of the agroecological transition. Modelling this transition requires considering both plant-plant interactions and plants' interactions with abiotic and biotic environments. Modelling crop mixtures enables designing ways to use plant diversity to provide ecosystem services, as long as they include crop management as input. A single modelling approach is not sufficient, however, and complementarities between models may be critical to consider the multiple processes and system components involved at different and relevant spatial and temporal scales. In this article, we present different modelling solutions implemented in a variety of examples to upscale models from local interactions to ecosystem services. We highlight that modelling solutions (i.e. coupling, metamodelling, inverse or hybrid modelling) are built according to modelling objectives (e.g. understand the relative contributions of primary ecological processes to crop mixtures, quantify impacts of the environment and agricultural practices, assess the resulting ecosystem services) rather than to the scales of integration. Many outcomes of multispecies agroecosystems remain to be explored, both experimentally and through the heuristic use of modelling. Combining models to address plant diversity and predict ecosystem services at different scales remains rare but is critical to support the spatial and temporal prediction of the many systems that could be designed

Erratum to: Genetic relationship between greisenization and Sn–W mineralizations in vein and greisen deposits: Insights from the Panasqueira deposit (Portugal)

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Dynamic Permeability Related to Greisenization Reactions in Sn-W Ore Deposits: Quantitative Petrophysical and Experimental Evidence

Massive greisens are commonly associated with Sn-W mineralization and constitute low-grade high-tonnage deposits. The formation of this type of deposit results from an intense pervasive metasomatic alteration involving a major fluid and mass transfer through a nominally impermeable parental granite. A decrease in the volume of the solid phases associated with the mineral replacement reactions may be a potential process for creating pathways to enhance fluid flow. Here, we explore the effects of the replacement reactions related to greisenization on the granite’s mineralogy and petrophysical properties (density, porosity, and permeability), as well as their potential implications for fluid flow in the case of the world-class Panasqueira W-Sn-(Cu) deposit, Portugal. Mineralogical and microtextural analyses of greisenized facies show that the total replacement of feldspars by muscovite is associated with a volume decrease of the solid phases that induces a significant porosity generation in greisen (~8.5%). Greisenization experiments coupled with permeability measurements show that the replacement of feldspars by muscovite permits new pathways at the crystal scale that significantly enhance the transient permeability. Moreover, permeability measurements performed on representative samples with different degrees of greisenization show that permeability increases progressively with the level of alteration from 10-20 m2 in least granite to 10-17 m2 in greisen. The correlation between the permeability and porosity evolutions demonstrates that the porous texture developed during replacement reactions creates new pathways that enhance significantly the permeability in greisen systems. The occurrences of mineral-bearing metals such as cassiterite in the newly formed porosity of greisen provide evidence that greisenization can be a decisive process for enhancing fluid flow and promoting transport of metals in Sn-W deposits. Finally, we present a model involving a positive feedback between greisenization and permeability, in which mineralizing fluids are able to generate their own pathways in initially impermeable granite via replacement reactions, which in turn promote further hydrothermal alteration and mass transport

On the morphology and amplitude of 2D and 3D thermal anomalies induced by buoyancy-driven flow within and around fault zones

International audienceIn the first kilometers of the subsurface, temperature anomalies due to heat conduction processes rarely exceed 20-30 • C. When fault zones are sufficiently permeable , fluid flow may lead to much larger thermal anomalies , as evidenced by the emergence of thermal springs or by fault-related geothermal reservoirs. Hydrothermal convec-tion triggered by buoyancy effects creates thermal anomalies whose morphology and amplitude are not well known, especially when depth-and time-dependent permeability is considered. Exploitation of shallow thermal anomalies for heat and power production partly depends on the volume and temperature of the hydrothermal reservoir. This study presents a non-exhaustive numerical investigation of fluid flow models within and around simplified fault zones, wherein realistic fluid and rock properties are accounted for, as are appropriate boundary conditions. 2D simplified models point out relevant physical mechanisms for geological problems, such as "ther-mal inheritance" or pulsating plumes. When permeability is increased, the classic "finger-like" upwellings evolve towards a "bulb-like" geometry, resulting in a large volume of hot fluid at shallow depth. In simplified 3D models wherein the fault zone dip angle and fault zone thickness are varied , the anomalously hot reservoir exhibits a kilometer-sized "hot air balloon" morphology or, when permeability is depth-dependent, a "funnel-shaped" geometry. For thick faults, the number of thermal anomalies increases but not the amplitude. The largest amplitude (up to 80-90 • C) is obtained for vertical fault zones. At the top of a vertical, 100 m wide fault zone, temperature anomalies greater than 30 • C may extend laterally over more than 1 km from the fault boundary. These preliminary results should motivate further geothermal investigations of more elaborated models wherein topography and fault intersections would be accounted for