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Petrogenesis of the Late Cenozoic volcanics of Hispaniola

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6070079
Late Cenozoic volcanic rocks of Hispaniola are subdivided into two geochemically contrasting series, a mafic alkaline series (MA-series) and a calc-alkaline series (CA-series). MA-series basalts show slight to moderate silica undersaturation, high TiO/sub 2/ and MgO contents and moderately high total alkalis. MA types are strongly enriched in K, Rb, Sr, Ba, U, Th and LREEs with Ba/La ratios of 0.98. REE patterns are highly fractionated (La/sub n//Yb/sub n/ ratios = 62, and La/sub n//Sm/sub n/ ratios = 6.3). HFS elements Zr, Hf, Nb and Ta are high resembling intraplate basalts. 87Sr/86Sr ratios are high (.7059 to .7079) with low Rb/Sr ratios (.03 to .15). The basalts, basaltic andesites, trachyandesites and dacites of the CA-series show lower TiO2 and MgO contents and moderately high total alkali contents. Strong enrichment is seen in K, Rb, Sr, Th, U and LREEs with Ba/La ratios as high as 5.6. REE patterns are fractionate to a lesser degree compared to the MA-series (average La/sub n//Yb/sub n/ = 23.4, and La/sub n//Sm/sub n/ ratios less than 5). HFS elements are lower resembling typical island arc types. CA-series show lower 87Sr/86Sr ratios (.7043 to .7053), with similarly low Rb/Sr ratios as seen in the MA-series. The MA-series and CA-series must have two separate primary sources as constrained by isotopic and trace element differences. Suggested models involve multi-stage, multi-component petrogenesis. Enrichment of depleted sub-arc mantle by a metasomatic melt fluid followed by second stage partial melting and final fractional crystallization are the principle elements of the preferred model.
Research Organization:
George Washington Univ., Washington, DC (USA)
OSTI ID:
6070079
Report Number(s):
CONF-8510489-
Conference Information:
Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
Country of Publication:
United States
Language:
English