초록 ▼

A method for forming a prograde kinematic model allowing reproduction in 3D intermediate geometries of geologic objects of an underground zone such as a sedimentary basin, from an initial state to a current state. A representation of the current geometry of the geologic objects of the zone is formed

A method for forming a prograde kinematic model allowing reproduction in 3D intermediate geometries of geologic objects of an underground zone such as a sedimentary basin, from an initial state to a current state. A representation of the current geometry of the geologic objects of the zone is formed by interpretation of acquired data obtained by seismic exploration, by in-situ measurements and by observations, then each geologic object is subdivided into layers separated by deformation interfaces. Each one of the layers is defined by means of a grid pattern into a series of hexahedral volume elements. Tectonic deformations are then applied separately and successively to each series of volume elements of a layer in relation to an underlying layer while conserving the thickness and the surface area of an intermediate neutral surface in each volume element. Then the tectonic deformations are iteratively modified until a geologic representation substantially in accordance with the known final state of the underground zone is obtained.

대표청구항 ▼

1. A method for forming a kinematic model allowing reproduction in 3D intermediate geometries of geologic objects of an underground zone, between an initial state and a known final state, the geometry of the geological objects of the zone being determined to be in the final state by interpretation o

1. A method for forming a kinematic model allowing reproduction in 3D intermediate geometries of geologic objects of an underground zone, between an initial state and a known final state, the geometry of the geological objects of the zone being determined to be in the final state by interpretation of acquired data obtained by seismic exploration, by in-situ measurements and by observations, comprising the steps of: a) subdividing each geologic object in the initial state thereof into layers, each layer being defined by a grid pattern into a series of hexahedral volume elements; b) applying separately and successively tectonic deformations to each series of the hexahedral volume elements of a layer in relation to an underlying layer with conservation of the thickness of the layer and conservation of the surface area of an intermediate neutral surface in each volume element so as to obtain a geological representation; c) comparing the geological representation and the final state of the underground zone; and d) iteratively modifying the initial state and repeating steps a) to c) until a geological representation substantially best fitting the final state of the underground zone is obtained. 2. A method as claimed in claim 1, comprising: subdividing each geologic object into layers separated from one another by deformation interfaces. 3. A method as claimed in claim 2, wherein: the deformation interfaces consist of the contact surfaces between the layers. 4. A method as claimed in claim 2, wherein: the deformation interfaces consist of intermediate ductile layers. 5. A method as claimed in claim 2, comprising: providing a geometrical modification of the grid patterns which accounts for the effects of compaction. 6. A method as claimed in claim 1, comprising: providing a geometrical modification of the grid patterns which accounts for the effects of compaction.