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- W1957047236 abstract "The Aluminum Saturation Index is related to the MgO/TiO2 ratio and both may be added to other typological parameters commonly used in the granitic series discrimination. Some well-known examples are listed and they lead to propose new geochemical limits characterizing different geodynamic settings. Four main groups may be recognized, 1: calc-alkaline granitoids (high Ca and low K) together with the island arc tholeiitic granitoids (ASI=1 for MgO=1.8% and MgO/TiO2 =2); 2: crustal peraluminous granitoids (ASI>1 and MgO/TiO2 = 3) produced in the collision zones; 3: tardi- and post-collision (K calc-alkaline) granitoids (ASI=1 for MgO=3.7% and MgO/TiO2 =4) and 4: the alkaline and peralkaline granitoids and the mid-ocean ridge tholeiitic granitoids emplaced in rifting or doming zones (ASI=1 for MgO=0.8% and MgO/TiO2=l)." @default.
- W1957047236 created "2016-06-24" @default.
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- W1957047236 date "1999-01-01" @default.
- W1957047236 modified "2023-09-28" @default.
- W1957047236 title "The aluminum saturation index and the MgO/TiO2 ratio: two parameters influenced by PH2O and discriminant in the magmatic series" @default.
- W1957047236 doi "https://doi.org/10.5327/rbg.v29i1.666" @default.
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