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中国科学技术大学地震学原理与应用课件 第三章(Part II)-d
中国科学技术大学 地震学原理 应用 课件 第三章 (Part II)-d
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2019/3/28
中国科学技术大学地震学原理与应用课件 第三章(Part II)-d。
中国科学技术大学地震学原理与应用课件 第三章(Part II)-c
中国科学技术大学 地震学原理 应用 课件 第三章 (Part II)-c
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2019/3/28
中国科学技术大学地震学原理与应用课件 第三章(Part II)-c。
中国科学技术大学地震学原理与应用课件 第三章(Part II)-b
中国科学技术大学 地震学原理 应用 课件 第三章 (Part II)-b
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2019/3/28
中国科学技术大学地震学原理与应用课件 第三章(Part II)-b。
中国科学技术大学地震学原理与应用课件 第三章(Part II)-a
中国科学技术大学 地震学原理 应用 课件 第三章 (Part II)-a
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2019/3/28
中国科学技术大学地震学原理与应用课件 第三章(Part II)-a。
中国科学技术大学地震学原理与应用课件 第三章(Part I)-d
中国科学技术大学 地震学 原理 应用 课件 第三章 (Part I)-d
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2019/3/28
中国科学技术大学地震学原理与应用课件 第三章(Part I)-d。
中国科学技术大学地震学原理与应用课件 第三章(Part I)-c
中国科学技术大学 地震学原理 应用 课件 第三章 (Part I)-c
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2019/3/28
中国科学技术大学地震学原理与应用课件 第三章(Part I)-c。
中国科学技术大学地震学原理与应用课件 第三章(Part I)-b
中国科学技术大学 地震学原理 应用 课件 第三章 (Part I)-b
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2019/3/28
中国科学技术大学地震学原理与应用课件 第三章(Part I)-b。
High-density macroseismic survey in urban areas. Part 1: proposal for a methodology and its application to the city of Rome
urban area high-density macroseismic survey questionnaire urban geology Rome
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2015/10/8
The aim of this research is to provide an original contribution to the investigation of local macroseismic variations in urban areas by means of questionnaire surveys. In this paper, we propose a meth...
Paleoseismology of the Yangsan Fault,southeastern part of the Korean Peninsula
Yangsan Fault (YSF) Korean Peninsula averge slip rate most recent event
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2015/9/16
The NNE-trending Yangsan Fault (YSF) is the most prominent fault in the southeastern part of the Korean Peninsula and has a continuous trace about 200 km long. Activity on this fault was recently inve...
Determination of volatiles in volcanic rocks and minerals with a Directly Coupled Evolved Gas Analyzing System (DEGAS) -Part I: Interpretation of degassing profiles (DEGAS-profiles) of minerals and rocks on the basis of melting experiments
volatiles magmatic rocks basaltic glass degassing Hawaiian lava remelting blacksand
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2015/9/10
Volatile components in magma strongly influence many physical properties of melts and minerals. The temperature
resolved degassing analysis of volcanic crystalline and vitreous rocks gives detailed i...
Stiffnites. Part II
Submarine sediment flows Magnetic fabric and anisotropy
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2015/8/27
The dynamics of a stiffnite are here inferred. A stiffnite is a sheet-shaped, gravity-driven submarine sediment flow, with a fabric made up of marine ooze. To infer stiffnite dynamics, order of magnit...
Stiffnites. Part I
Submarine gravity-driven sediment flows landslide and asteroid tsunamis
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2015/8/27
I identify the early phases of a particular kind of gravity-driven submarine sediment flow, that I have named immature stiffnite. The mature flow dynamics is originally presented in an accompanying re...
Wave-equation-based travel-time seismic tomography – Part 2: Application to the 1992 Landers earthquake (Mw 7.3) area
High resolution 3 d P wave S wave crust velocity poisson's ratio model landers earthquake earthquake fault
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2015/1/6
High-resolution 3-D P and S wave crustal velocity and Poisson's ratio models of the 1992 Landers earthquake (Mw 7.3) area are determined iteratively by a wave-equation-based travel-time seismic tomogr...
Wave-equation-based travel-time seismic tomography – Part 1: Method
Travel seismic tomography step by step linearity sensitivity to the kernel
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2015/1/6
In this paper, we propose a wave-equation-based travel-time seismic tomography method with a detailed description of its step-by-step process. First, a linear relationship between the travel-time resi...
Fully probabilistic seismic source inversion – Part 1: Efficient parameterisation
Earthquake source inversion seismology non-linear uncertainty parameters the bayesian
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2015/1/6
Seismic source inversion is a non-linear problem in seismology where not just the earthquake parameters themselves but also estimates of their uncertainties are of great practical importance. Probabil...