ALKALINE AND CALC-ALKALINE BASALTS FROM CAPULIN MOUNTAIN, NORTHEASTERN NEW MEXICO, U.S.A.

Significance of hornblende in calc-alkaline andesites and basalts

Hornblende occurs in some andesitic and basaltic rocks of calc-alkaline affini1y, where it is commonly associated with olivine. The texture, eruption history, and composition are interpreted to indicate that hornblende commonly forms as a product of reaction between olivine and basaltic and andesitic liquids. The natural hornblendes probably formed within the crust at temperatures between 960o ...

Transition from Paleogene Normal Calc-Alkaline to Neogene Adakitic-Like Plutonism and

Chitinolytic bacteria from alkaline hypersaline Mono Lake, California, USA

Chitinolytic activity was detected in sediment and water-column samples from Mono Lake, California, USA, using fluorogenic analogues. In order to learn more about chitin degradation in Mono Lake, we analyzed the phylogenetic composition of bacterial assemblages in chitin-enrichment cultures and associated with Artemia monica exuvia. We also isolated chitinolytic bacteria from aerobic and anaero...

transition from paleogene normal calc-alkaline to neogene adakitic-like plutonism and

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High-Mg# andesitic lavas of the Shisheisky Complex, Northern Kamchatka: implications for primitive calc-alkaline magmatism

Primitive arc magmatism and mantle wedge processes are investigated through a petrologic and geochemical study of high-Mg# (Mg/Mg ? Fe [ 0.65) basalts, basaltic andesites and andesites from the Kurile-Kamchatka subduction system. Primitive andesitic samples are from the Shisheisky Complex, a field of Quaternary-age, monogenetic cones located in the Aleutian–Kamchatka junction, north of Shiveluc...