Underwater Relief and Sediments in the Area of the St. Petersburg Mud Volcano (Lake Baikal)

IF 0.3 Q4 GEOGRAPHY
N. A. Gubin, E. E. Kononov, A. S. Poletaev, A. G. Chensky
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引用次数: 0

Abstract

A combined analysis is made of the structure of the St. Petersburg mud volcano and the lake bottom surface surrounding it using bathymetric, seismoacoustic, backscatter, and water column data. A high-precision digital elevation model with a horizontal resolution of up to 10 m has been developed for the bottom surface in the area of the volcano. By analyzing the resulting model, it is possible to update the morphometric parameters of the underwater structure under consideration and prepare a detailed morphological description. It has been found that the volcanic edifice consists of several ridgelike parts located on the wings of the Gidratnyi Fault and crossing it. A canyon-shaped and curved in plan 800-m wide valley was mapped to the southeast of the fault. A graphical representation of backscatter data with separation by types of sedimentary layers is created via a comparison of the intensity of the reflected signal and expected mathematical model values. Based on the results of data analysis, it has been established that the mud volcano mainly consists of clay with the possible inclusion of relatively large fragments (up to 10 cm). Presumably there are also large fragments on the bottom surface around the volcano; however, fine-grained fractions (sandy, clayey, and silty) are dominant. A three-dimensional visualization of the water column data is presented for the study area with the detected outcrops of gas in the form of two gas flares with the observed heights of 800 and 700 m. According to a statistical sample of the values of the reflected signal amplitudes, the intensity of gas release in the flares differs by approximately 7 times. The seismoacoustic data of the chirp profiler indicate the possible presence of gas hydrates.

Abstract Image

圣彼得堡泥火山(贝加尔湖)水下地形与沉积物
摘要利用测深、地震声、后向散射和水柱资料,对圣彼得堡泥火山及其周围湖底表面的结构进行了综合分析。在该火山地区的底面建立了一个水平分辨率高达10米的高精度数字高程模型。通过分析得到的模型,可以更新所考虑的水下结构的形态计量参数,并准备详细的形态描述。已经发现,火山大厦由几个山脊状的部分组成,这些部分位于吉德拉尼断层的两翼上,并穿过断层。在断层的东南方,绘制了一个800米宽的峡谷形弧形山谷。通过将反射信号的强度与预期的数学模型值进行比较,创建了按沉积层类型分离的后向散射数据的图形表示。根据数据分析的结果,泥火山主要由粘土组成,可能包含较大的碎片(达10厘米)。据推测,火山周围的底部表面也有大块碎片;然而,细粒组分(砂质、粘土和粉砂质)占主导地位。对研究区水柱数据进行了三维可视化处理,发现了两个气焰形式的天然气露头,观测高度分别为800和700 m。根据反射信号振幅值的统计样本,耀斑中气体释放的强度相差约7倍。啁啾剖面仪的地震声学数据表明可能存在天然气水合物。
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来源期刊
CiteScore
0.50
自引率
0.00%
发文量
24
期刊介绍: Geography and Natural Resources  publishes information on research results in the field of geographical studies of nature, the economy, and the population. It provides ample coverage of the geographical aspects related to solving major economic problems, with special emphasis on regional nature management and environmental protection, geographical forecasting, integral regional research developments, modelling of natural processes, and on the advancement of mapping techniques. The journal publishes contributions on monitoring studies, geographical research abroad, as well as discussions on the theory of science.
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