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Titlebook: Electrical Properties of the Earth’s Mantle; Wallace H. Campbell Book 1987 Springer Basel AG 1987 ANOVA.Enzo Paci.Greenhouse.MCD.boundary

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书目名称Electrical Properties of the Earth’s Mantle
编辑Wallace H. Campbell
视频video
丛书名称Pageoph Topical Volumes
图书封面Titlebook: Electrical Properties of the Earth’s Mantle;  Wallace H. Campbell Book 1987 Springer Basel AG 1987 ANOVA.Enzo Paci.Greenhouse.MCD.boundary
描述Table 1 Earth conductivity profiles Figure File Name Apx. Depth Remarks References 1. Global Models 1939-69 LAPR39 0--1250 global Sq, Dst LAHIRI and PRICE, 1939; PRICE, 1973 RIKI50 0--1400 misc. data sources RIKITAKE. 1950; 1966 MCD057 0--2900 LAPR39 + secular change McDoNALD, 1957 CANT60 100--600 see ECKHARDT et a!. , 1963 CANTWELL, 1960 YUKU65 380--1900 ring current YUKUTAKE, 1965 BANK69 0--1700 ring current BANKS, 1969; 1972 2. Global Models 1970--74 BFRS70 100--700 Sq, Dst 27-d variations BERDICHEVSKY et a!. , 1970; 1973 PRKR70 0--3200 rework BANKS, 1969, data PARKER, 1970 SCJA72 0--1000 pulsations, bays, Sq, Dst SCHMUCKER and JANKOWSKI, 1972 BANK72 230--1250 model summary BANKS, 1972 JADY74 0--2951 Sq, 27-d, annual variations JADY, 1974 FAR074 300--1500 with BFRS70 FAINBERG and ROTANOVA, 1974 SCHM74 0--1000 see HAAK, 1980 SCHMUCKER, 1974 DMRB77 0--1450 all available data DMITRIEV et al. , 1977 Global Models 1974-1983 3. PRKN74 60-430 Sq PARKINSON, 1974 DUCM80 0--2900 annual means DUCRUIX et a!. , 1980 ISIK80 320--2020 Sq, Dst, annual, solar cycle ISIKARA, 1980 ACMC81 0--2875 secular impulse ACACHE et a!. , 1980 ROKI82 350--1200 various methods ROKITYANSKY. 1982 JAPA83 0--1200
出版日期Book 1987
关键词ANOVA; Enzo Paci; Greenhouse; MCD; boundary element method; earth; lithosphere; model; parkinson; solar; value
版次1
doihttps://doi.org/10.1007/978-3-0348-7373-4
isbn_softcover978-3-0348-7375-8
isbn_ebook978-3-0348-7373-4Series ISSN 2504-3625 Series E-ISSN 2504-3633
issn_series 2504-3625
copyrightSpringer Basel AG 1987
The information of publication is updating

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MTS Studies on the Upper Mantle Conductivity in China,ayer is basically consistent with the low velocity zone in the upper mantle, and Cenozoic tectonism and current seismicity are significantly related to the variation of depth of the conductive layer in the upper mantle. The possible origins of the conductive layers in the upper mantle have been discussed here.
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Die kosmischen Nebel und Sternhaufeninuity, bounds the crust and the ‘upper mantle’. Between about 100 and 220 km deep, a low velocity zone is encountered beyond which the velocity increases continuously and in steps near 400, 670, and perhaps 770 km. The name ‘lower mantle’ is assigned to the region from about 1000 km to the start of the core at 2890 km deep.
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2504-3625 HIRI and PRICE, 1939; PRICE, 1973 RIKI50 0--1400 misc. data sources RIKITAKE. 1950; 1966 MCD057 0--2900 LAPR39 + secular change McDoNALD, 1957 CANT60 100--600 see ECKHARDT et a!. , 1963 CANTWELL, 1960 YUKU65 380--1900 ring current YUKUTAKE, 1965 BANK69 0--1700 ring current BANKS, 1969; 1972 2. Globa
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