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   <subfield code="D">G.</subfield>
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   <subfield code="a">Il microgabbro in val cavallina (pezzaze, prealpi bresciane): Caratteri chimici e mineralogici</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[G. Schiavinato]</subfield>
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   <subfield code="a">Chemical and mineralogical characters of a microgabbro plug in Val Cavallina (Pezzaze, Prealps)</subfield>
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   <subfield code="a">Not far from Brescia, a microgabbro plug crops out within the Southern Alpine Basement schists, next to the Val Trompia Line, an important extensional lineament of Variscan age which underwent compressive reactivation during Alpine age. The rock type shows ophitic texture and is composed of calcic clinopyroxene of diopside type and sodic plagioclase, minor Ti-rich biotite; accessory minerals are apatite, Fe-Ti oxides and zircon. Secondary minerals as epidote, Ti-poor biotite, sericite, chlorite, and plagioclase with anomalous composition are ascribed to post-magmatic alteration processes. The geochemical characteristics of the rock indicate moderate SiO2 undersaturation and alkali enrichment. According to the primary mineral association, the rock type may be ascribed to a mildly alkaline series. Immobile elements suggest the emplacement of the plug in a within-plate geodynamic environment. The time relationship between the microgabbro plug and the Permian and Triassic magmatites outcropping in the adiacent areas need to be better known.</subfield>
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