کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4692322 1636792 2013 16 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Stochastic velocity inversion of seismic reflection/refraction traveltime data for rift structure of the southwest Barents Sea
ترجمه فارسی عنوان
معکوس سرعت اتفاقی داده های زمان بندی بازتاب / لرزش لرزه ای برای ساخت رفته در جنوب غربی دریای بارنتز
کلمات کلیدی
دریای بارنتز، حاشیه تبدیل، رختکن قاره ای، ساختار پوسته، مدل سازی سرعت انکسار بازتابی، کشش و نازک شدن عوامل
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• Crustal velocity structure reflects multi-stage rifting in the SW Barents Sea.
• A stochastic inversion is applied to the widely-used RAYINVR raytracing package.
• β factors peak 200 km landward of the transform margin edge.
• Maximum β coincides with Caledonian suture.
• We determine 227 ± 16 km total extension of the Barents Sea rifted margin.

We present results from an active-source, onshore–offshore seismic reflection/refraction transect acquired as part of the PETROBAR project (Petroleum-related studies of the Barents Sea region). The 700 km-long profile is oriented NW–SE, coincident with previously published multichannel seismic reflection profiles. We utilize layer-based raytracing in a Markov Chain Monte Carlo (MCMC) inversion to determine a probabilistic velocity model constraining the sedimentary rocks, crystalline crust, and uppermost mantle in a complex tectonic regime. The profile images a wide range of crustal types and ages, from Proterozoic craton to Paleozoic to early Cenozoic rift basins; and volcanics related to Eocene continental breakup with Greenland. Our analyses indicate a complex architecture of the crystalline crust along the profile, with crystalline crustal thicknesses ranging from 43 km beneath the Varanger Peninsula to 12 km beneath the Bjørnøya Basin. Assuming an original, post-Caledonide crustal thickness of 35 km in the offshore area, we calculate the cumulative thinning (β) factors along the entire profile. The average β factor along the profile is 1.7 ± 0.1, suggesting 211–243 km of extension, consistent with the amount of overlap derived from published plate reconstructions. Local β factors approach 3, where Bjørnøya Basin reaches a depth of more than 13 km. Volcanics, carbonates, salt, diagenesis and metamorphism make deep sedimentary basin fill difficult to distinguish from original, pre-rift crystalline crust, and thus actual stretching may in places exceed our estimates.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volume 593, 8 May 2013, Pages 135–150
نویسندگان
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