New PDF release: Benthic Foraminiferal Biostratigraphy of the South Caribbean

By H. M. Bolli, J.-P. Beckmann, J. B. Saunders

This ebook offers an important info set for benthic foraminifera present in the vintage southern Caribbean area. It assembles facts on a thousand of crucial species for the time span Cretaceous to Miocene (120 to ten million years sooner than present). Age levels are put in the framework of these used for planktic foraminifera present in Plankton Stratigraphy (Bolli et al., CUP, 1985). The taxa were cited so far generically, and in lots of circumstances new comparisons between species were made--the overdue Cretaceous and Early Paleogene are relatively particular. this data, including targeted illustrations, will let the taxa for use stratigraphically.

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1994). , 1996, 1997). 3), rather than invoking effusion rates that are orders of magnitude larger than any documented eruption. One recent model attempts to incorporate elements of both fast and slow emplacement to explain the CRB (Reidel, 1998). The inflation mechanism has applications to flows other than just those of basalts or LIPs. Ultramafic komatiite flows have compositions suggestive of very fluid lava (see Chapter 8), but komatiites typically are quite old and preserved evidence of flow emplacement is often difficult to find.

1987), which is directly related to the intensity of energy release associated with a hydromagmatic eruption (Sheridan and Wohletz, 1983). 3. Fountain-Fed Rhyolitic Eruptions Fire-fountaining is commonly considered an eruptive mode confined to basalts and other mafic magma compositions with relatively low viscosities, but an increasing number of rhyolitic units are interpreted to have fonned by fountaining. They range from small welded tephra rings through moderately sized secondary lava flows to widespread welded airfall tuffs that blanket any preeruptive topography (Christiansen and Blank, 1975; Duffield, 1990; Manley, 1994; Christiansen, in press; Manley and Mclntosh, in press), and are known primarily from Yellowstone National Park in Wyoming, southwestern New Mexico, and southwestern Idaho, all in the United States.

McBimey, A. , Conductivity variations and terrestrial heat-flow distribution, J Geophys. , 68, 6323-6329, 1963. McSween, H. Y, What we have learned about Mars from SNC meteorites, Meteoritics, 29, 757-779, 1994. , and W G. Melson, Nuees ardentes of the 1968 eruption of Mayon volcano, Philippines, Bull. , 33,600-620, 1969. , and A. R. McBimey, Properties of some common igneous rocks and their melts at this temperature, Geo/. Soc. Am. , 84, 3563-3592, 1973. , Prentice-Hall, Englewood Cliffs, NJ, 1996.

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