SU1056099A1 - Seismic danger determination method - Google Patents

Seismic danger determination method Download PDF

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Publication number
SU1056099A1
SU1056099A1 SU823391633A SU3391633A SU1056099A1 SU 1056099 A1 SU1056099 A1 SU 1056099A1 SU 823391633 A SU823391633 A SU 823391633A SU 3391633 A SU3391633 A SU 3391633A SU 1056099 A1 SU1056099 A1 SU 1056099A1
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SU
USSR - Soviet Union
Prior art keywords
seismic
temperature
propagation
measured
layer
Prior art date
Application number
SU823391633A
Other languages
Russian (ru)
Inventor
Керим Мамедхан оглы Керимов
Ариф Гасанович Гасанов
Христофор Паноиотович Метакса
Аркадий Нисонович Пильчин
Яков Нисонович Пильчин
Азай Гурбатович Рзаев
Original Assignee
Общественная Творческая Конструкторская Лаборатория "Гея" Центра Методологии Изобретательства
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Priority to SU823391633A priority Critical patent/SU1056099A1/en
Application granted granted Critical
Publication of SU1056099A1 publication Critical patent/SU1056099A1/en

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    • G—PHYSICS
    • G01—MEASURING; TESTING
    • G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
    • G01V1/01—Measuring or predicting earthquakes

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  • Physics & Mathematics (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • Engineering & Computer Science (AREA)
  • Acoustics & Sound (AREA)
  • Environmental & Geological Engineering (AREA)
  • Geology (AREA)
  • Remote Sensing (AREA)
  • General Life Sciences & Earth Sciences (AREA)
  • General Physics & Mathematics (AREA)
  • Geophysics (AREA)
  • Measurement Of Mechanical Vibrations Or Ultrasonic Waves (AREA)

Abstract

СПОСОБ ОПРЕДЕЛЕНИЯ СЕЙСМИЧЕСКОЙ ОПАСНОСТИ, включающий измерение скорости распространени упругой вопны с заоанной частотой в исспеЩгемом слое сейсмттческой зоны, отличающийс  тем, что, с цепью повышени  достоверности прогноза сейсмической опасности, измер ют температуру иСспецуемого сло  сейсмической зоны, провоц т измерение скорооти распрострешени  упругой волны с той же частотой в образце горной пороцы, характеризующем исследуемый слой, при зацанной величине напр жений и измерен . ной температуре, и по превышению скорости распространени  упругой волны в исследуемом слое величины скорости i распространени  упругой волны в образце горной породы суд т о наличии сей (Л смической опасности в сейсмической зоне .A METHOD FOR DETERMINING SEISMIC HAZARD, including measuring the velocity of propagation of elastic matter with a common frequency in the test layer of the seismic zone, characterized in that, with a chain to improve the reliability of the prediction of seismic hazard, measure the temperature of the discharge layer of the seismic zone, test gear, which is a part of the target area. the same frequency in the sample of rock porous, which characterizes the layer under study, with measured voltages, is measured. This temperature is determined by the presence of the elastic temperature in the sample of the rock in excess of the velocity of propagation of the elastic wave in the layer under study (i) in a seismic zone.

Description

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QD СОQD WITH

Claims (1)

СПОСОБ ОПРЕДЕЛЕНИЯ СЕЙСМИЧЕСКОЙ ОПАСНОСТИ, включаю- щий измерение скорости распространенияупругой волны с заданной частотой в исследуемом слое сейсмической зоны, отличающийся тем, что, с цепью повышения достоверности прогноза сейсмической опасности, измеряют температуру исследуемого слоя сейсмической зоны, проводят измерение скорооти распространения упругой волны с той же частотой в образце горной породы, характеризующем исследуемый спой, при заданной величине напряжений и измерен. ной температуре, и по превышению скорости распространения упругой волны в исследуемом слое величины скорости распространения упругой волны в образце горной породы судят о наличии сейсмической опасности в сейсмической эоне.METHOD FOR DETERMINING SEISMIC DANGERS, including measuring the propagation velocity of an elastic wave with a given frequency in the studied layer of the seismic zone, characterized in that, with the chain of increasing the reliability of the forecast of the seismic hazard, the temperature of the studied layer of the seismic zone is measured, the propagation velocity of the elastic wave is measured from the same frequency in a rock specimen characterizing the studied spoil at a given value of stress and measured. temperature, and by exceeding the speed of propagation of the elastic wave in the studied layer, the values of the speed of propagation of the elastic wave in the rock sample are judged on the presence of seismic hazard in the seismic aeon. SU „„1056099SU „„ 1056099
SU823391633A 1982-04-30 1982-04-30 Seismic danger determination method SU1056099A1 (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
SU823391633A SU1056099A1 (en) 1982-04-30 1982-04-30 Seismic danger determination method

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
SU823391633A SU1056099A1 (en) 1982-04-30 1982-04-30 Seismic danger determination method

Publications (1)

Publication Number Publication Date
SU1056099A1 true SU1056099A1 (en) 1983-11-23

Family

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Family Applications (1)

Application Number Title Priority Date Filing Date
SU823391633A SU1056099A1 (en) 1982-04-30 1982-04-30 Seismic danger determination method

Country Status (1)

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SU (1) SU1056099A1 (en)

Non-Patent Citations (1)

* Cited by examiner, † Cited by third party
Title
1, Сейсмическое просвечивание очаговых зон. М., изц-во ИФЗ АН СССР, 1977, с. 171-1-94. 2. Исспецовани по физике земпетр :сений. М., Наука, 1976, с. 217-236/ (прототип). *

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