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首页> 外文期刊>Doklady Earth Sciences >Age of the Shirshov Submarine Ridge Basement (Bering Sea) Based on the Results of Investigation of Zircons Using the U-Pb SHRIMP Method
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Age of the Shirshov Submarine Ridge Basement (Bering Sea) Based on the Results of Investigation of Zircons Using the U-Pb SHRIMP Method

机译:基于U-Pb SHRIMP方法对锆石的调查结果,确定了舍尔肖夫海底海底地下室的年龄(白令海)

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The Shirshov Ridge holds an important position in the structure of the Bering Sea Basin. Stretching from north to south for over 500 km, it divides the Bering Sea into two deep water basins, the Aleutian and Komandorsky basins. The age of oceanic crust of the Aleutian basin based on linear magnetic anomalies is conventionally considered Early Cretaceous, of the Komandorsky basin — Miocene, according to the K—Ar dating of the basalts (9.8 Ma) exposed in 191 deep water drill borehole. Rocks belonging to the basement of the Shirshov Ridge were dredged during the 29th cruise of research vessel Dmitrii Mendeleev and are represented by amphibolitic gabbro whose composition is similar to that of gabbroids of mid-oceanic ridges. The age of metamorphism based on the results of K—Ar dating of amphibole is 47 ± 5 Ma. The U-Pb zircon dating method was used to determine the age of gabbro. Zircons were extracted from a ~5 kg combined amphibolitic gabbroid sample, and the age of zircons was determined using a SHRIMP—II sensitive high resolution secondary ion microprobe (Center of Isotopic Studies, A.P. Karpinskii Russian Geological Research Institute, St. Petersburg). The average concordant age value for the 25 determinations performed based on 20 points for 18 grains is 72 ± 1.4 Ma (Late Campanian). For 5 grains, the measured age values are within the range of 88 ± 3.5 Ma to 126.5 ± 4.5 Ma. Given the western vergence of the thrust structure of the Shirshov Ridge, the acoustic basement of the Shirshov Ridge is most probably a complexly deformed oceanic crust of the Aleutian Trench, which most likely dates from the Early to Late Cretaceous.%Geological Institute, Russian Academy of Sciences, 7 Pyzhevskiiper., Moscow, 119017 Russia;Geological Institute, Russian Academy of Sciences, 7 Pyzhevskiiper., Moscow, 119017 Russia;International Institute of Earthquake Prognosis Theory and Mathematical Geophysics, Russian Academy of Sciences, 84/32 ul. Profsoyuznaya, Moscow, 117997 Russia;A. P. Karpinskii Russian Geological Research Institute, 74 Sredniipr., St. Petersburg, 199106 Russia;A. P. Karpinskii Russian Geological Research Institute, 74 Sredniipr., St. Petersburg, 199106 Russia;
机译:Shirshov山脊在白令海盆地的结构中占有重要地位。它从北向南延伸超过500公里,将白令海分为两个深水盆地,即阿留申盆地和科曼多斯基盆地。根据在191个深水钻探钻孔中暴露的玄武岩(9.8 Ma)的K-Ar年代,通常认为基于线性磁异常的阿留申盆地洋壳年龄是Komandorsky盆地中新世的早白垩纪。在第29艘研究船Dmitrii Mendeleev航行期间,疏通了属于Shirshov山脊地下室的岩石,并以闪石长辉岩为代表,其组成与中洋脊的辉石相似。根据角闪石的K-Ar测年结果得出的变质年龄为47±5 Ma。用U-Pb锆石测年法确定辉长岩的年龄。从约5千克的混合角闪石辉石样样品中提取锆石,并使用SHRIMP-II敏感的高分辨率次级离子微探针(同位素研究中心,A.P。Karpinskii俄罗斯地质研究所,圣彼得堡)确定锆石的年龄。基于18个谷物的20分进行的25次测定的平均一致年龄值为72±1.4 Ma(坎帕尼晚期)。对于5粒谷物,测得的年龄值在88±3.5 Ma至126.5±4.5 Ma的范围内。考虑到Shirshov山脊逆冲构造的西部集中性,Shirshov山脊的声学基底很可能是阿留申海沟复杂变形的洋壳,最有可能是早于白垩纪到晚白垩纪。%科学院,莫斯科117,俄罗斯,热那夫斯基; 119017俄罗斯;俄罗斯科学院地质研究所,俄罗斯,119017,热那亚,莫斯科;俄罗斯科学院国际地震预测理论和数学地球物理研究所,84/32 ul。莫斯科,Profsoyuznaya,117997俄罗斯; A。 P.Karpinskii俄罗斯地质研究院,圣彼得堡Sredniipr。74,199106俄罗斯; A。 P. Karpinskii俄罗斯地质研究院,俄罗斯圣彼得堡74 Sredniipr。,199106;

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  • 来源
    《Doklady Earth Sciences》 |2011年第1期|p.926-932|共7页
  • 作者单位

    Geological Institute, Russian Academy of Sciences, 7 Pyzhevskiiper., Moscow, 119017 Russia;

    Geological Institute, Russian Academy of Sciences, 7 Pyzhevskiiper., Moscow, 119017 Russia;

    International Institute of Earthquake Prognosis Theory and Mathematical Geophysics, Russian Academy of Sciences, 84/32 ul. Profsoyuznaya, Moscow, 117997 Russia;

    A. P. Karpinskii Russian Geological Research Institute, 74 Sredniipr., St. Petersburg, 199106 Russia;

    A. P. Karpinskii Russian Geological Research Institute, 74 Sredniipr., St. Petersburg, 199106 Russia;

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