A Generalized Model of Filtration in a Fractured-Porous Medium with Low-Permeable Inclusions and Its Possible Applications     

Lobkovskii  L. I.  Ramazanov  M. M. 《Izvestiya Physics of the Solid Earth》2022,58(2):281-290

Izvestiya, Physics of the Solid Earth - Abstract—This work generalizes the classical mathematical model of fluid and gas filtration in a fractured-porous medium. It results in a generalized...  相似文献   

Variations of Natural Electrical Potentials in the Cryolithozone,Yakutsk     

Kozlov  V. I.  Baishev  D. G.  Pavlov  E. A. 《Izvestiya Physics of the Solid Earth》2022,58(3):435-442

Izvestiya, Physics of the Solid Earth - Abstract—This paper considers daily, seasonal, and interannual variations of natural potentials at two sites in the cryolithozone at the testing...  相似文献   

Assessment of the Seismic Situation in the Region of Greece’s Eastern Coast of the Aegean Sea before the Earthquake with M = 6.7 (October 30, 2020)     

Popandopoulos  G. A. 《Izvestiya Physics of the Solid Earth》2022,58(3):346-363

Izvestiya, Physics of the Solid Earth - Abstract—A detailed study has been carried out regarding temporal variations of seismicity in the region of Greece’s eastern coast of the Aegean...  相似文献   

Erratum to: The Khuvsgul Earthquake of January 12, 2021 (MW = 6.7, ML = 6.9) and Early Aftershocks     

Emanov  A. F.  Emanov  A. A.  Chechel’nitskii  V. V.  Shevkunova  E. V.  Radziminovich  Ya. B.  Fateev  A. V.  Kobeleva  E. A.  Gladyshev  E. A.  Arapov  V. V.  Artemova  A. I.  Podkorytova  V. G. 《Izvestiya Physics of the Solid Earth》2022,58(3):443-443

Izvestiya, Physics of the Solid Earth - An Erratum to this paper has been published: https://doi.org/10.1134/S1069351322100019  相似文献   

Erratum to: Seasonal Variations in the b-Value of the Reservoir-Triggered Seismicity in the Koyna–Warna Region,Western India     

Smirnov  V. B.  Potanina  M. G.  Kartseva  T. I.  Ponomarev  A. V.  Patonin  A. V.  Mikhailov  V. O.  Sergeev  D. S. 《Izvestiya Physics of the Solid Earth》2022,58(4):603-603

Izvestiya, Physics of the Solid Earth - An Erratum to this paper has been published: https://doi.org/10.1134/S1069351322090014  相似文献   

Mapping soil liquefaction susceptibility across Europe using the analytic hierarchy process     

Meisina  C.  Bonì  R.  Bozzoni  F.  Conca  D.  Perotti  Cesare  Persichillo  Pina  Lai  C. G. 《Bulletin of Earthquake Engineering》2022,20(11):5601-5632

Bulletin of Earthquake Engineering - Mapping the susceptibility of earthquake-induced soil liquefaction at the continental scale is a challenge. Susceptibility of soils to liquefaction is the...  相似文献   

Spectral wave characteristics in the coastal waters of the central west coast of India during tropical cyclone Kyarr     

Nair  M. Anjali  Amrutha  M. M.  Kumar  V. Sanil 《Ocean Dynamics》2022,72(2):151-168

Ocean Dynamics - The study presents the assessment of spectral wave conditions in the coastal waters of the central west coast of India based on data from waverider buoys at two locations during...  相似文献   

The hydrodynamic theory of the Cyprus Eddy     

Egorova  Viktoriia M.  Zyryanov  Valery N.  Sokolovskiy  Mikhail A. 《Ocean Dynamics》2022,72(1):1-20

Ocean Dynamics - An analytical solution to the problem of the Cyprus warm core Eddy generation over the bottom topography non-axisymmetric perturbations in the broad area of the Eratosthenes...  相似文献   

In situ calcite U−Pb geochronology by high-sensitivity single-collector LA-SF-ICP-MS     

Wu  Shitou  Yang  Yueheng  Roberts  Nick M. W.  Yang  Ming  Wang  Hao  Lan  Zhongwu  Xie  Bohang  Li  Tianyi  Xu  Lei  Huang  Chao  Xie  Liewen  Yang  Jinhui  Wu  Fuyuan 《中国科学:地球科学(英文版)》2022,65(6):1146-1160

Science China Earth Sciences - U?Pb geochronology of calcite using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) is an emerging method, with potential applications...  相似文献   

Under the surface: Pressure-induced planetary-scale waves,volcanic lightning,and gaseous clouds caused by the submarine eruption of Hunga Tonga-Hunga Ha'apai volcano     

David A. Yuen  Melissa A. Scruggs  Frank J. Spera  Yingcai Zheng  Hao Hu  Stephen R. McNutt  Glenn Thompson  Kyle Mandli  Barry R. Keller  Songqiao Shawn Wei  Zhigang Peng  Zili Zhou  Francesco Mulargia  Yuichiro Tanioka 《地震研究进展（英文）》2022,2(3):100134

We present a narrative of the eruptive events culminating in the cataclysmic January 15, 2022 eruption of Hunga Tonga-Hunga Ha'apai Volcano by synthesizing diverse preliminary seismic, volcanological, sound wave, and lightning data available within the first few weeks after the eruption occurred. The first hour of eruptive activity produced fast-propagating tsunami waves, long-period seismic waves, loud audible sound waves, infrasonic waves, exceptionally intense volcanic lightning and an unsteady volcanic plume that transiently reached—at 58 ?km—the Earth's mesosphere. Energetic seismic signals were recorded worldwide and the globally stacked seismogram showed episodic seismic events within the most intense periods of phreatoplinian activity, and they correlated well with the infrasound pressure waveform recorded in Fiji. Gravity wave signals were strong enough to be observed over the entire planet in just the first few hours, with some circling the Earth multiple times subsequently. These large-amplitude, long-wavelength atmospheric disturbances come from the Earth's atmosphere being forced by the magmatic mixture of tephra, melt and gasses emitted by the unsteady but quasi-continuous eruption from 0402±1–1800 UTC on January 15, 2022. Atmospheric forcing lasted much longer than rupturing from large earthquakes recorded on modern instruments, producing a type of shock wave that originated from the interaction between compressed air and ambient (wavy) sea surface. This scenario differs from conventional ideas of earthquake slip, landslides, or caldera collapse-generated tsunami waves because of the enormous (～1000x) volumetric change due to the supercritical nature of volatiles associated with the hot, volatile-rich phreatoplinian plume. The time series of plume altitude can be translated to volumetric discharge and mass flow rate. For an eruption duration of ～12 ?h, the eruptive volume and mass are estimated at 1.9 ?km³ and ～2 900 ?Tg, respectively, corresponding to a VEI of 5–6 for this event. The high frequency and intensity of lightning was enhanced by the production of fine ash due to magma—seawater interaction with concomitant high charge per unit mass and the high pre-eruptive concentration of dissolved volatiles. Analysis of lightning flash frequencies provides a rapid metric for plume activity and eruption magnitude. Many aspects of this eruption await further investigation by multidisciplinary teams. It represents a unique opportunity for fundamental research regarding the complex, non-linear behavior of high energetic volcanic eruptions and attendant phenomena, with critical implications for hazard mitigation, volcano forecasting, and first-response efforts in future disasters.  相似文献