標(biāo)題: Titlebook: Electrical Properties of the Earth’s Mantle; Wallace H. Campbell Book 1987 Springer Basel AG 1987 ANOVA.Enzo Paci.Greenhouse.MCD.boundary [打印本頁] 作者: Fillmore 時(shí)間: 2025-3-21 18:49
書目名稱Electrical Properties of the Earth’s Mantle影響因子(影響力)
書目名稱Electrical Properties of the Earth’s Mantle影響因子(影響力)學(xué)科排名
書目名稱Electrical Properties of the Earth’s Mantle網(wǎng)絡(luò)公開度
書目名稱Electrical Properties of the Earth’s Mantle網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Electrical Properties of the Earth’s Mantle被引頻次
書目名稱Electrical Properties of the Earth’s Mantle被引頻次學(xué)科排名
書目名稱Electrical Properties of the Earth’s Mantle年度引用
書目名稱Electrical Properties of the Earth’s Mantle年度引用學(xué)科排名
書目名稱Electrical Properties of the Earth’s Mantle讀者反饋
書目名稱Electrical Properties of the Earth’s Mantle讀者反饋學(xué)科排名
作者: Blood-Clot 時(shí)間: 2025-3-21 22:31
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.作者: reflection 時(shí)間: 2025-3-22 02:06 作者: 儀式 時(shí)間: 2025-3-22 07:39 作者: 背帶 時(shí)間: 2025-3-22 08:53 作者: 極微小 時(shí)間: 2025-3-22 16:54
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.作者: 極微小 時(shí)間: 2025-3-22 17:02 作者: languor 時(shí)間: 2025-3-23 00:21 作者: expansive 時(shí)間: 2025-3-23 03:03 作者: 敲竹杠 時(shí)間: 2025-3-23 09:01
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作者: 圍巾 時(shí)間: 2025-3-23 13:17
Die Untersuchungsmethoden des Auges,servations. For areas characterized by different tectonic settings and very large lateral variations, a discussion is made about structural models based on seismological, geothermal and electrical conductivity data.作者: Suppository 時(shí)間: 2025-3-23 15:39 作者: Encapsulate 時(shí)間: 2025-3-23 19:14 作者: 我怕被刺穿 時(shí)間: 2025-3-23 22:44 作者: 連鎖 時(shí)間: 2025-3-24 06:21 作者: 主動(dòng)脈 時(shí)間: 2025-3-24 10:19 作者: 大門在匯總 時(shí)間: 2025-3-24 11:25
The Upper Mantle Conductivity Analysis Method Using Observatory Records of the Geomagnetic Field,ion techniques employed. This review of the Sq-analysis features critical to a conductivity derivation is pictorially presented along with the equations for application of the . (1970) technique to the . coefficients for a conductivity determination. Three examples illustrate the use of these equations with different .. models.作者: Cognizance 時(shí)間: 2025-3-24 15:27
Book 1987RICE, 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 1作者: poliosis 時(shí)間: 2025-3-24 19:20
Die Erkrankungen des Sehnerven, cpd. These responses are presented as the potential ratio ., depth of penetration . and apparent resistivity ... The data are compared to, and included with, other global response estimates and the combined data used to derive model earth conductivity profiles by linear, nonlinear and Monte-Carlo inversion techniques.作者: 投射 時(shí)間: 2025-3-25 03:10
Die Untersuchungsmethoden des Auges,lues covering periods from 6 hours up to 11 years is compiled. With the help of averaged data of the magnetovariation sounding a planetary geoelectric profile is constructed meeting the requirements of up-to-date understanding of the physical processes in the Earth.作者: 蜈蚣 時(shí)間: 2025-3-25 04:17
Grundriss der Augenheilkunde für Studierendebservatories supply sufficient accurate data, and their distribution on the Earth is very irregular. More importantly, the assumption implicit in deep conductivity determinations, that the conductivity is a function of depth only, breaks down because of near surface conductivity anomalies.作者: 斷斷續(xù)續(xù) 時(shí)間: 2025-3-25 07:42
Conductivity Profiles from Global Data, cpd. These responses are presented as the potential ratio ., depth of penetration . and apparent resistivity ... The data are compared to, and included with, other global response estimates and the combined data used to derive model earth conductivity profiles by linear, nonlinear and Monte-Carlo inversion techniques.作者: Eulogy 時(shí)間: 2025-3-25 11:40
Models of Deep Electrical Conductivity Obtained From Data on Global Magnetic Variational Sounding,lues covering periods from 6 hours up to 11 years is compiled. With the help of averaged data of the magnetovariation sounding a planetary geoelectric profile is constructed meeting the requirements of up-to-date understanding of the physical processes in the Earth.作者: 發(fā)誓放棄 時(shí)間: 2025-3-25 16:28
Limitations in the Use of Spherical Harmonic Methods for Deep Conductivity Determinations,bservatories supply sufficient accurate data, and their distribution on the Earth is very irregular. More importantly, the assumption implicit in deep conductivity determinations, that the conductivity is a function of depth only, breaks down because of near surface conductivity anomalies.作者: 消音器 時(shí)間: 2025-3-25 20:39 作者: 陳舊 時(shí)間: 2025-3-26 02:31
978-3-0348-7375-8Springer Basel AG 1987作者: Small-Intestine 時(shí)間: 2025-3-26 07:17
Electrical Properties of the Earth’s Mantle978-3-0348-7373-4Series ISSN 2504-3625 Series E-ISSN 2504-3633 作者: 圖畫文字 時(shí)間: 2025-3-26 12:33 作者: 有罪 時(shí)間: 2025-3-26 13:57 作者: 農(nóng)學(xué) 時(shí)間: 2025-3-26 19:55
Das wellenmechanische Bild des Atomsocity structure is determined. Analysis procedures include ray theory calculations and synthetic seismograms computed using reflectivity techniques. The P wave velocity structure beneath the Canadian Shield is virtually identical to that beneath the Baltic Shield to a depth of at least 800 km. Two m作者: Overstate 時(shí)間: 2025-3-26 23:29
Die Untersuchungsmethoden des Auges,of intensive research work. We present a summary of results based on the inversion of available surface-wave dispersion data and .-wave travel time observations. For areas characterized by different tectonic settings and very large lateral variations, a discussion is made about structural models bas作者: 壓迫 時(shí)間: 2025-3-27 03:12
,Die Erkrankungen der Tr?nenorgane,ntial for any interpretation of magnetotelluric data in projecting lithospheric structural models. The measured values of the terrestrial heat flow, radiogenic heat production, and thermal conductivity of rocks allow the extrapolation of surface observations to a greater depth and the calculation of作者: 哎呦 時(shí)間: 2025-3-27 08:54 作者: 地牢 時(shí)間: 2025-3-27 12:48
Die Erkrankungen der Bindehaut,pherically symmetric model of the electrical conductivity. The existing induction data have been supplemented by about 80 new values derived from the analysis of daily means. The fit of the existing 1-D models of the electrical conductivity of the mantle to the set of induction data is investigated.作者: 疾馳 時(shí)間: 2025-3-27 15:49
,Die Erkrankungen der Tr?nenorgane,6h-24h period range. We use associate directions and we eliminate the effects of deviation of telluric currents. We thus obtain for each observatory reliable phases and apparent resistivity values representative of the neighbouring stratified substratum. It appears that the values obtained in the fo作者: 聰明 時(shí)間: 2025-3-27 20:33 作者: somnambulism 時(shí)間: 2025-3-27 22:27 作者: 柔聲地說 時(shí)間: 2025-3-28 03:37
Die Erkrankungen des Sehnerven, cpd. These responses are presented as the potential ratio ., depth of penetration . and apparent resistivity ... The data are compared to, and included with, other global response estimates and the combined data used to derive model earth conductivity profiles by linear, nonlinear and Monte-Carlo i作者: aggrieve 時(shí)間: 2025-3-28 08:49
Die Untersuchungsmethoden des Auges,lues covering periods from 6 hours up to 11 years is compiled. With the help of averaged data of the magnetovariation sounding a planetary geoelectric profile is constructed meeting the requirements of up-to-date understanding of the physical processes in the Earth.作者: LIMIT 時(shí)間: 2025-3-28 13:38 作者: Ambulatory 時(shí)間: 2025-3-28 18:06
Grundriss der Augenheilkunde für Studierendebservatories supply sufficient accurate data, and their distribution on the Earth is very irregular. More importantly, the assumption implicit in deep conductivity determinations, that the conductivity is a function of depth only, breaks down because of near surface conductivity anomalies.作者: Complement 時(shí)間: 2025-3-28 21:31 作者: 有組織 時(shí)間: 2025-3-28 23:31
Geobotanik (Pflanzengeographie),n. This paper presents a review of some theoretical techniques for determining both the vertical and horizontal conductivity profiles of a region using a spatial distribution of observed electromagnetic fields at the Earth’s surface. Effects of shallow positioned anomalies upon a deep conductivity d作者: 枯燥 時(shí)間: 2025-3-29 03:43
Crustal and Upper Mantle Structure of Stable Continental Regions in North America and Northern Eurole analysis using many record sections is described. The S wave velocity structure beneath the Canadian Shield is derived from constrained surface wave data. The thickness of the lithosphere beneath the Canadian and Baltic Shields is determined to be 95–100 km. The continental plate thickness may be作者: 旅行路線 時(shí)間: 2025-3-29 08:58
Temperature Profiles in the Earth of Importance to Deep Electrical Conductivity Models, and upper mantle rocks within the interval 200–1,000°C. It is shown how the knowledge of the temperature field can be used in the evaluation of the deep electrical conductivity pattern by converting the conductivity-versus-temperature data into the conductivity-versus-depth data.作者: muffler 時(shí)間: 2025-3-29 14:29
Upper Mantle Lateral Heterogeneities and Magnetotelluric Daily Variation Data,al melting or percentage of fluids of the upper mantle: at depths of about 300 km, the upper mantle appears to be 100 C hotter under Australia than under Europe; the probable presence of fluids at depths about 100 km in the southwesiern North America upper mantle appears to be responsible for the hi作者: 遷移 時(shí)間: 2025-3-29 16:24 作者: NOVA 時(shí)間: 2025-3-29 22:05
Book 1987 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 作者: 舊式步槍 時(shí)間: 2025-3-30 03:10
2504-3625 q, 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 978-3-0348-7375-8978-3-0348-7373-4Series ISSN 2504-3625 Series E-ISSN 2504-3633 作者: 進(jìn)入 時(shí)間: 2025-3-30 05:34
Das wellenmechanische Bild des Atomsle analysis using many record sections is described. The S wave velocity structure beneath the Canadian Shield is derived from constrained surface wave data. The thickness of the lithosphere beneath the Canadian and Baltic Shields is determined to be 95–100 km. The continental plate thickness may be作者: echnic 時(shí)間: 2025-3-30 12:11 作者: 饒舌的人 時(shí)間: 2025-3-30 12:54 作者: Hemiparesis 時(shí)間: 2025-3-30 17:17 作者: 矛盾 時(shí)間: 2025-3-30 22:06 作者: Frisky 時(shí)間: 2025-3-31 03:10 作者: esthetician 時(shí)間: 2025-3-31 07:55
Properties of the Lithosphere-Asthenosphere System in Europe with a View Toward Earth Conductivity,of intensive research work. We present a summary of results based on the inversion of available surface-wave dispersion data and .-wave travel time observations. For areas characterized by different tectonic settings and very large lateral variations, a discussion is made about structural models bas
