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首页> 外文期刊>Annals Of Geophysics >Acquisition and preliminary analysis of multi-channel seismic reflection data, acquired during the oceanographic cruises of the TOMO-ETNA experiment
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Acquisition and preliminary analysis of multi-channel seismic reflection data, acquired during the oceanographic cruises of the TOMO-ETNA experiment

机译:在TOMO-ETNA实验的海洋航行中获取和初步分析了多通道地震反射数据

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The TOMO-ETNA experiment was performed in the framework of the FP7 “MED-SUV” (MEDiterranean SUpersite Volcanoes) in order to gain a detailed geological and structural model of the continental and oceanic crust concerning Etna and Aeolian Islands volcanoes (Sicily, Italy), by means of active and passive seismic exploration methodologies. Among all data collected, some 1410 km of marine multi-channel seismic (MCS) reflection profiles were acquired in the Ionian and Tyrrhenian Seas during two of the three oceanographic cruises of the TOMO-ETNA experiment, in July and November 2014, with the aim of shading light to deep, intermediate and shallow stratigraphy and crustal structure of the two above mentioned areas. The MCS sections, targeted to deep exploration, were acquired during the oceanographic cruise on board the R/V “Sarmiento de Gamboa”, using an active seismic source of 16 air-guns, for a total volume of 4340 cu. in., and a 3000 m long, 240-channels digital streamer as receiving system. High-resolution seismic profiles were instead collected through the R/V “Aegaeo”, using two smaller air-guns (overall 270 cu. in. volume) and a 96 channels, 300 m long digital streamer. This paper provides a detailed description of the acquisition parameters and main processing steps adopted for the MCS data. Some processed lines are shown and preliminarily interpreted, to highlight the overall good quality and the high potential of the MCS sections collected during the TOMO-ETNA experiment.
机译:TOMO-ETNA实验是在FP7“ MED-SUV”(地中海超现场火山)的框架内进行的,目的是获得有关埃特纳火山和风神群岛火山(意大利西西里岛)的大陆和海洋硬壳的详细地质结构模型,采用主动和被动地震勘探方法。在2014年7月和11月的TOMO-ETNA实验的三次海洋航行中,有两次在爱奥尼亚海和第勒尼安海采集了所有收集到的数据,其中约1410 km是海洋多通道地震反射剖面,目的是阴影对上述两个地区的深,中,浅地层和地壳结构的影响。 MCS部分是针对深度勘探的,是在“ Sarmiento de Gamboa” R / V上进行海洋航行时获得的,使用了16支气枪的主动地震震源,总体积为4340 cu。英寸和3000 m长的240通道数字流媒体作为接收系统。取而代之的是使用两个较小的气枪(总容积为270 cu。in。)和96通道,300 m长的数字拖缆,通过R / V“ Aegaeo”收集高分辨率地震剖面。本文详细介绍了MCS数据的采集参数和主要处理步骤。显示并初步解释了一些加工线,以突出显示TOMO-ETNA实验期间收集的MCS切片的整体质量和高潜力。

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