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Description: La mappa strutturale mostra una classificazione degli assi di anticlinale in funzione del più giovane orizzonte deformato (sulla base del modello geologico 3D), e delle faglie in funzione del più giovane orizzonte sicuramente tagliato. Per maggiori dettagli fare riferimento al Report del Progetto "GeoMol" ALPINE SPACE PROGRAMME e al Rapporto dell'area pilota Mantova-Brescia.

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Layer: SEISMICITY AND ACTIVE STRESS (5)

Sub Layers:
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• insSEISM25p
• insSEISp
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Description: La mappa mostra: la sismicità storica (dal Catalogo CPTI11 di INGV; http://emidius.mi.ingv.it/CPTI11/) rappresentata da quadrati di dimensioni proporzionali alla magnitudo dell'evento; la sismicità strumentale per il periodo 1990-2015 (da Database ISIDe di INGV; http://iside.rm.ingv.it/) rappresentata da cerchi di dimensioni proporzionali alla magnitudo, per magnitudo superiore/uguale a 2.5, e da cerchi di uguale dimensione per magnitudo inferiori; l'orientazione dei vettori dello stress orizzontale massimo (Shmax) ottenuti attraverso l'applicazione web SHINE (http://shine.rm.ingv.it/index.phtml), mediante interpolazione su una griglia con passo 0.1° dei dati tratti dal database del World Stress Map Project (http://dc-app3-14.gfz-potsdam.de/). Per maggiori dettagli fare riferimento al Report del Progetto "GeoMol" ALPINE SPACE PROGRAMME e al Rapporto dell'area pilota Mantova-Brescia.

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Layer: axSHMAXp (6)

Parent Layer: SEISMICITY AND ACTIVE STRESS

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Layer: ACTIVE FAULTS AND SEISMOGENIC SOURCES (10)

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• regCSSf
• topCSSgeol
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Description: La mappa mostra in scala di colori le variazioni di gravità effetto delle variazioni laterali di densità; anomalie positive (colori caldi) indicano aree con valori medi di densità maggiori del valore di calcolo, mentre le anomalie negative (colori freddi) si riscontrano in aree a minore densità. Le isolinee hanno equidistanza di 2 mGal. La mappa è stata ottenuta elaborando dati ENI presenti nella banca dati geofisica di ISPRA ed è il risultato di un filtro passa alto della mappa di anomalie di Bouguer calcolato alla densità di 2.6 g/cm3. Per maggiori dettagli fare riferimento al Report del Progetto "GeoMol" ALPINE SPACE PROGRAMME e al Rapporto dell'area pilota Mantova-Brescia.

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