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Shear waves from three-component ocean bottom seismographs off Lofoten, Norway, indicative of anisotropy in the lower crust

机译：从挪威洛菲登的三分海洋底部地震仪剪切波，指示下皮中的各向异性

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Rolf Mjelde;
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年度 1992
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1. A regional shear-wave velocity model in the central Voring basin, N. Norway, using three-component ocean bottom seismographs [J] . Digranes P., Kodaira S., Shimamura H., Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth . 1998,第3a4期

机译：使用三分量海底地震仪的挪威北部中央瓦尔灵盆地的区域横波速度模型
2. Shear wave anisotropy of laminated lower crust beneath Urach (SW Germany): a comparison with xenoliths and with exposed lower crustal sections [J] . Rabbel W., Seiss T., Pohl M., Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth . 1998,第4期

机译：Urach（德国西南部）下层状下部地壳的剪切波各向异性：与异岩和下部地壳裸露部分的比较
3. The effect of a hydrous phase on P-wave velocity anisotropy within a detachment shear zone in the slow-spreading oceanic crust: A case study from the Godzilla Megamullion, Philippine Sea [J] . Michibayashi Katsuyoshi, Watanabe Tohru, Harigane Yumiko, The island arc . 2016,第3期

机译：含水相对缓速扩散大洋地壳剥离剪切带内P波速度各向异性的影响：以菲律宾哥斯拉巨Mega为例
4. Extraction of crustal deformations and oceanic fluctuations from ocean bottom pressures [C] . Keisuke Ariyoshi, Hiroyuki Matsumoto, Takeshi Iinuma, OCEANS 2016 MTS/IEEE Monterey . 2016

机译：从海底压力中提取地壳变形和海洋波动
5. Geochemical investigation of the lower crustal rocks in Bamble Shear Belt, southern Norway: Implications for the source of gold in lode gold deposits. [D] . Alirezaei, Saeed. 2000

机译：挪威南部Bamble Shear Belt下地壳岩石的地球化学研究：对金矿床中金的含意。
6. Ocean-Bottom Seismographs Based on Broadband MET Sensors: Architecture and Deployment Case Study in the Arctic [O] . Artem A. Krylov, Ivan V. Egorov, Sergey A. Kovachev, 2021

机译：基于宽带的海底地震仪达到传感器：北极地区建筑和部署案例研究
7. Possible shallow crustal shear wave anisotropy off Lofoten, Norway, inferred from three-component ocean-bottom seismographs [O] . Rolf Mjelde, Markvard A. Sellevoll 1993

机译：可能的浅地壳剪切波各向异性，挪威洛菲特，从三组分海底地震仪推断出来

Shear waves from three-component ocean bottom seismographs off Lofoten, Norway, indicative of anisotropy in the lower crust

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