کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
5787369 | 1641475 | 2017 | 14 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Inferences on the lithospheric structure of Campi Flegrei District (southern Italy) from seismic noise cross-correlation
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موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فیزیک زمین (ژئو فیزیک)
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چکیده انگلیسی
The distribution of VS shows a pyroclastic covering with VS increasing from 0.3-0.7Â km/s to 2.1Â km/s. It rests on a lava or carbonate basement, about 5-6Â km thick, with VS increasing from 2.1Â km/s to 3.1Â km/s at about 2Â km of depth and rising to â¼0.6Â km towards the island of Procida. A metamorphic layer is detected at an average depth of 7.7Â km with VS of 3.8-3.9Â km/s, about 5Â km thick, overlying a low velocity layer (VS of 3.5Â km/s) at about 11-12Â km of depth. The VS model along the ISCHIA-MIS path, as average of the models obtained by combining local and regional dispersion data of the two adjoining cells, is well consistent with the other paths. The Moho discontinuity is retrieved at about 23Â km of depth with VS of 4.2Â km/s.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Physics of the Earth and Planetary Interiors - Volume 265, April 2017, Pages 92-105
Journal: Physics of the Earth and Planetary Interiors - Volume 265, April 2017, Pages 92-105
نویسندگان
M.R. Costanzo, C. Nunziata,