کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4691411 1636728 2016 13 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Evidence for anomalous mantle upwelling beneath the Arabian Platform from travel time tomography inversion
ترجمه فارسی عنوان
شواهد نشان می دهد که آپاندیسیت گوشته انحصاری زیر پلتفرم عربستان از معکوس توموگرافی زمان سفر است
کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• A new upper mantle tomographic model is constructed for the Arabian Plate region.
• The derived anomalies fit the major structural units of the region.
• A low-velocity anomaly beneath the Arabian Plate traces a mantle upwelling.
• This hot area was responsible for the origin of recent volcanism in Western Arabia.
• A high velocity beneath the Red Sea may indicate a passive rifting mechanism.

We present a new model of P-velocity anomalies in the upper mantle beneath the Arabian Peninsula, Red Sea, and surrounding regions. This model was computed with the use of travel time data from the global catalogue of the International Seismological Center (ISC) for the years of 1980–2011. The reliability of the model was tested with several synthetic tests. In the resulting seismic model, the Red Sea is clearly associated with a higher P-velocity anomaly in the upper mantle at least down to 300 km depth. This anomaly might be caused by upward deviation of the main mantle interfaces caused by extension and thinning of the lithosphere due to passive rifting. Thick lithosphere of the Arabian Platform is imaged as a high-velocity anomaly down to 200–250 km depth. Below this plate, we observe a low-velocity structure that is interpreted as a hot mantle upwelling. Based on the tomography results, we propose that this upper mantle anomaly may represent hot material that migrates westward and play a major role in the formation of Cenozoic basaltic lava fields in western Arabia. On the northeastern side of the Arabian Plate, we clearly observe a dipping high-velocity zone beneath Zagros and Makran, which is interpreted as a trace of subduction or delamination of the Arabian Plate lithosphere.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volume 667, 23 January 2016, Pages 176–188
نویسندگان
, , , , , ,