SU1589230A1 - Method of seismic investigations of deposits of oil and gas - Google Patents
Method of seismic investigations of deposits of oil and gas Download PDFInfo
- Publication number
- SU1589230A1 SU1589230A1 SU884409398A SU4409398A SU1589230A1 SU 1589230 A1 SU1589230 A1 SU 1589230A1 SU 884409398 A SU884409398 A SU 884409398A SU 4409398 A SU4409398 A SU 4409398A SU 1589230 A1 SU1589230 A1 SU 1589230A1
- Authority
- SU
- USSR - Soviet Union
- Prior art keywords
- oil
- seismic
- gas
- filters
- carried out
- Prior art date
Links
Landscapes
- Geophysics And Detection Of Objects (AREA)
Abstract
Изобретение относитс к сейсмическим методам исследовани месторождений нефти и газа и может быть использовано при разведке вы вленных структур с целью прогнозировани и определени контура нефтегазоносности. Цель изобретени - повышение эффективности. Дл этого производитс одновременна регистраци микросейсмических колебаний сетью сейсмический станций, расположенных в пределах и вне контура месторождени . Наблюдени провод тс в течение не менее 5 сут. двум раздельными частотными каналами в диапазоне частот от 0,5 до 2 Гц, причем фильтраци осуществл етс неперекрывающимис полуоктавными фильтрами. Строитс зависимость отношение амплитуд на выходах двух частотных каналов от месторождени пункта регистрации. Аномали графика отношений соответствует положению месторождени .The invention relates to seismic methods for the exploration of oil and gas fields and can be used in the exploration of identified structures in order to predict and determine the oil and gas content contour. The purpose of the invention is to increase efficiency. For this, simultaneous recording of microseismic vibrations by a network of seismic stations located within and outside the field contour is performed. The observations are carried out for at least 5 days. two separate frequency channels in the frequency range from 0.5 to 2 Hz, and filtering is carried out by non-overlapping semi-octave filters. The dependence of the amplitudes at the outputs of the two frequency channels on the field of the registration point is constructed. Anomalies of the relationship chart corresponds to the position of the field.
Description
Изобретение относитс к сейсмическим методам исследовани месторождений нефти и газа и может быть использовано при разведке вы вленных структур с целью прогнозировани и определени контура нефтегазоноснос- ти.The invention relates to seismic methods for studying oil and gas fields and can be used in the exploration of identified structures in order to predict and determine the contour of oil and gas content.
Цель изобретени - повышение эффективности .The purpose of the invention is to increase efficiency.
Способ осуществл ют следующим образом .The method is carried out as follows.
Наблюдени на излучаемых площад х ведут вдоль профилей, пересекающих сводовую часть структуры вкрест её простирани , с уплотнением пунктов наблюдений в сводовой части. Прот женность профилей выбирают такой, чтобыObservations on the radiated areas are along profiles that intersect the arched part of the structure across its strike, with a seal of observation points in the arched part. The length of the profiles is chosen so that
не менее двух крайних пунктов регистрации находились за пределами предполагаемого месторождени . Регистрацию вертикальной и горизонтальных компонент микросейсм ведут одновременно всеми сейсмическими станци ми на всей площади наблюдений в течение не менее 5 днейat least two extreme points of registration were outside the intended field. Vertical and horizontal components of microseisms are simultaneously recorded by all seismic stations over the entire observation area for at least 5 days.
Така продолжительность наблюдений обусловлена тем, что длительность аномалий микросейсмического фона различной природы (микросейсмические бури, техногенна де тельность и т.д ) ;не превышает 2-3 сут. В этом случае на врем регистрации ( не менее 5 сут.) приходитс достаточно продолжительный интервал времени, неSuch a duration of observations is due to the fact that the duration of anomalies of a microseismic background of different nature (microseismic storms, man-made activity, etc.) does not exceed 2-3 days. In this case, at the time of registration (at least 5 days) there is a rather long interval of time, not
зан тый аномалией микросейсмического фона, по которому можно уверенно выделить искомую аномалию, обусловленную нефтегазовой залежью. Регистрацию ведут одновременно двум частотно-разделенными каналами, Фильтра- даю зарегестрированных колебаний провод т с помощью двух полуоктавньгх фильтров с неперекрывающимис частотными полосами в диапазоне частот 0,5 - 2,0 Гц.occupied by the anomaly of the microseismic background, by which one can confidently isolate the desired anomaly caused by the oil and gas reservoir. The recording is carried out simultaneously by two frequency-separated channels. The filtering of registered oscillations is carried out with the help of two semi-octave filters with non-overlapping frequency bands in the frequency range 0.5-2.0 Hz.
Такой выбор обусловлен тем, что Ьклон частотной характеристики микро- сейсм, обеспечивающий получение надеж йых результатов, расположён в диапазоне частот 0,5 - 2 Гц. Частоты ниже 0,5 Гц плохо регистрируютс стандартными сейсмографами, а выше 2 Гц параметры микросейсм отличаютс неустойчивостью . При регистрации микро- 1сейсм с помощью автономных сейсмических станций с магнитной записью указанна фильтраци производитс при воспроизведении.Such a choice is due to the fact that the slope of the frequency response of a micro seismic, which provides reliable results, is located in the frequency range of 0.5 - 2 Hz. Frequencies below 0.5 Hz are poorly recorded with standard seismographs, and above 2 Hz, microseism parameters are unstable. When registering a micro-seismic with the help of autonomous seismic stations with magnetic recording, this filtering is performed during playback.
Затем дл каждого пункта регистрации определ ют отношени среднеквадратичных амплитуд, равные A(f,)/A(f2 где f и f 2 - соответственно нижн и верхн частоты, и стро т огибаю111ие этого отношени вдоль профилей наблюдений . Такой подход избавл ет от необходимости индентификации каналов регистрации. При пересечении контура нефтегазоносности. по мере приближени к сводовой части залежи увеличиThen, for each registration point, ratios of rms amplitudes equal to A (f,) / A are determined (f2 where f and f 2 are the lower and upper frequencies, respectively, and plot this ratio along the observation profiles. This approach eliminates the need for identification registration channels.When crossing the contour of oil and gas, as you approach the arch part of the reservoir,
00
5five
00
5five
ваютс значени отношений, св занные с увеличением поглощени на частоте fj . По точкам, соответствующим увеличению отношений, выдел ют примерный контур .месторождени .relationship values are associated with an increase in absorption at frequency fj. At the points corresponding to an increase in the ratio, an approximate contour of the place of birth is selected.
Использование изобретени обеспечивает повышение эффективности за счет меньшей зависимости от вариаций микросейсм во времени и в пространств е.The use of the invention provides an increase in efficiency due to less dependence on variations of microseisms in time and in space.
Claims (1)
Priority Applications (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
SU884409398A SU1589230A1 (en) | 1988-04-13 | 1988-04-13 | Method of seismic investigations of deposits of oil and gas |
Applications Claiming Priority (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
SU884409398A SU1589230A1 (en) | 1988-04-13 | 1988-04-13 | Method of seismic investigations of deposits of oil and gas |
Publications (1)
Publication Number | Publication Date |
---|---|
SU1589230A1 true SU1589230A1 (en) | 1990-08-30 |
Family
ID=21368380
Family Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
SU884409398A SU1589230A1 (en) | 1988-04-13 | 1988-04-13 | Method of seismic investigations of deposits of oil and gas |
Country Status (1)
Country | Link |
---|---|
SU (1) | SU1589230A1 (en) |
Cited By (1)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
EP0455091A2 (en) * | 1990-04-28 | 1991-11-06 | Koji Tokimatsu | Methods for measurement, analysis and assessment of ground structure |
-
1988
- 1988-04-13 SU SU884409398A patent/SU1589230A1/en active
Non-Patent Citations (1)
Title |
---|
Патент GB № 2174809, , кл. G 01 V 1/36,1986. Программа Развитие физических основ сейсмических методов. М:ИФЗ АН СССР, 1981, с. 158-160. * |
Cited By (3)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
EP0455091A2 (en) * | 1990-04-28 | 1991-11-06 | Koji Tokimatsu | Methods for measurement, analysis and assessment of ground structure |
EP0845688A3 (en) * | 1990-04-28 | 1998-07-29 | Koji Tokimatsu | System and method for measurement, analysis and assessment of ground structures |
US6253870B1 (en) | 1990-04-28 | 2001-07-03 | Koji Tokimatsu | Methods for measurement, analysis and assessment of ground structure |
Similar Documents
Publication | Publication Date | Title |
---|---|---|
Hartzell et al. | Initial investigation of site and topographic effects at Robinwood Ridge, California | |
Ferrazzini et al. | Characteristics of seismic waves composing Hawaiian volcanic tremor and gas‐piston events observed by a near‐source array | |
Shi et al. | Variability of crustal attenuation in the northeastern United States from Lg waves | |
Woolery et al. | Near‐surface deformation in the New Madrid Seismic zone as imaged by high resolution SH‐wave seismic methods | |
MXPA05003593A (en) | Method for separating microseismic signals from seismic signals emitted by one or several sources. | |
Gupta et al. | Broadband F‐K analysis of array data to identify sources of local scattering | |
Li et al. | Source properties of two microearthquakes at Kilauea volcano, Hawaii | |
SU1589230A1 (en) | Method of seismic investigations of deposits of oil and gas | |
Suhadolc et al. | A theoretical study of the dependence of the peak ground acceleration on source and structure parameters | |
Del Pezzo et al. | Velocity and spectral characteristics of the volcanic tremor at Etna deduced by a small seismometer array | |
Hagerty et al. | Observations at Costa Rican volcano offer clues to causes of eruptions | |
Furumoto et al. | Seismic image of the volcanic tremor source at Izu-Oshima volcano, Japan | |
Tsuruga et al. | Spatial and temporal variations of volcanic earthquakes at Sakurajima Volcano, Japan | |
Bonamassa et al. | Directional site resonances and the influence of near‐surface geology on ground motion | |
Iio | Seismic source spectrum of microearthquakes | |
Ukawa | Excitation mechanism of large-amplitude volcanic tremor associated with the 1989 Ito-oki submarine eruption, central Japan | |
NISHIGAMI et al. | Microseismic Activity and Spatial Distribution of Coda-Q in the Westernmost Part of the North Anatolian Fault Zone, Turkey | |
Knapp | Observations of the air-coupled wave as a function of depth | |
Yamasato et al. | Earthquake Swarm and Volcanic Tremors off Eastern Izu Peninsula in 1989 Spectral Investigation and Characteristics of Waveforms | |
Saito et al. | Precursory Change of Spectral Characteristics before the 1978 Miyagi-ken-oki Earthquake | |
Gao et al. | Studies of earthquakes on and near the Lop Nor, China, nuclear test site | |
Howell Jr | Lake Superior seismic experiment: Frequency spectra and absorption1 | |
Babcock | Microphone suppression of air-noise on geophones | |
Randall et al. | Array analysis of the large-aperture array of the 1988–89 PASSCAL Basin and Range Passive-Source Seismic Experiment | |
Murumatu et al. | Synthesis of strong motions by using an aftershock record as the Green's function |