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The Middle‐Upper Miocene Bodrum magmatic complex of the Aegean region, southwestern Turkey, is mainly represented by intermediate stocks, lavas, pyroclastic and volcaniclastic deposits. Monzonitic stocks and connected porphyry intrusions and extrusions are the first products of the magmatism. These are followed by a volcanic succession consisting of andesitic‐latitic lavas, autobrecciated lavas, pyroclastic and volcaniclastic deposits. The final stage is represented by basaltic and basaltic andesitic flows and dykes intruded into previous units. The volcanic succession crops out in the northern part of the Bodrum peninsula. In the lower part of this succession are widespread pyroclastic deposits, composed of pyroclastic fall and flow units, alternating with epiclastic deposits. Grain size, volume and thickness of the pyroclastic deposits were mainly controlled by the type, magnitude and intensity of the eruption. Further up the section, there are two horizons of debris avalanche deposits forming the coarsest and thickest deposits of the volcaniclastic succession. The debris avalanche deposits indicate at least two different flank collapses coeval with the volcanism. The stratigraphy and map pattern of these volcanic units imply that the northern part of the Bodrum peninsula was the north‐facing flank of a stratovolcano during the mid‐Late Miocene. Copyright © 2006 John Wiley & Sons, Ltd.  相似文献   

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《Geoarchaeology》2004,19(6):613-613
The original article to which this Erratum refers was published in Geoarchaeology 19(3), 2004, 185–218. Due to an oversight, authorship of the paper by Bassett, K.N., Gordon, H.W., Nobes, D.C., & Jacomb, C. (2004), “Gardening at the edge: Documenting the limits of tropical Polynesian kumara horticulture in southern New Zealand” (Geoarchaeology 19, No. 3, pp. 185–218), was assigned incorrectly. The correct authorship is Hamish W. Gordon, Kari N. Bassett, David C. Nobes, and Chris Jacomb. The authors apologize for this error.  相似文献   

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