MÉTODOS PARA MONITORAR UMA FORMAÇÃO DE SUB-SUPERFÍCIE ABAIXO DE UM LEITO MARINHO E PARA PRODUZIR HIDROCARBONETOS A PARTIR DE UMA FORMAÇÃO DE SUB-SUPERFÍCIE ABAIXO DE UM LEITO MARINHO

A method of detecting a lateral boundary of a compacting or expanding region in a subsurface formation, which method comprises determining non-vertical deformation of the earth' s surface above the subsurface formation over a period of time; identifying at least on contraction area and at least...

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Hauptverfasser: STEPHEN JAMES BOURNE, PAUL JAMES HATCHELL
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creator STEPHEN JAMES BOURNE
PAUL JAMES HATCHELL
description A method of detecting a lateral boundary of a compacting or expanding region in a subsurface formation, which method comprises determining non-vertical deformation of the earth' s surface above the subsurface formation over a period of time; identifying at least on contraction area and at least one adjacent dilatation area of the earth' s surface from the non-vertical deformation over the period of time; and using the contraction area and the adjacent dilatation area as an indication of a lateral boundary of the compacting or expanding region; and a method for producing hydrocarbons.
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identifying at least on contraction area and at least one adjacent dilatation area of the earth' s surface from the non-vertical deformation over the period of time; and using the contraction area and the adjacent dilatation area as an indication of a lateral boundary of the compacting or expanding region; and a method for producing hydrocarbons.</abstract><oa>free_for_read</oa></addata></record>
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subjects DETECTING MASSES OR OBJECTS
EARTH DRILLING
EARTH DRILLING, e.g. DEEP DRILLING
FIXED CONSTRUCTIONS
GEOPHYSICS
GRAVITATIONAL MEASUREMENTS
MEASURING
MINING
OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR ASLURRY OF MINERALS FROM WELLS
PHYSICS
TESTING
title MÉTODOS PARA MONITORAR UMA FORMAÇÃO DE SUB-SUPERFÍCIE ABAIXO DE UM LEITO MARINHO E PARA PRODUZIR HIDROCARBONETOS A PARTIR DE UMA FORMAÇÃO DE SUB-SUPERFÍCIE ABAIXO DE UM LEITO MARINHO
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