FAULTING AND TEXTURE CHANGES IN CHALK - AN EXAMPLE IN A GRABEN OF THE MONS BASIN (BELGIUM)

被引：0

作者：

GAVIGLIO, P

DALBISSIN, MC

BERGERAT, F

VANDYCKE, S

机构：

[1] UNIV PARIS 06, TECTON QUANTITAT LAB, CNRS, URA 1315, F-75252 PARIS 05, FRANCE

[2] FAC POLYTECH MONS, GEOL FONDAMENTALE & APPL LAB, FNRS, B-7000 MONS, BELGIUM

来源：

BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE | 1993年 / 164卷 / 04期

关键词：

FAULTS; EXTENSION TECTONICS; CHALK; POROSITY; COMPACTION; PRESSURE-SOLUTION AND CEMENTATION; THERMAL DILATATION; MONS BASIN;

D O I：

暂无

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Changes in texture of chalk are in close relationship with normal fault slips : porosity loss and decrease in pore size under compaction and pressure-solution and cementation. Fluids play a major part in the rearrangement of grains or in removal and deposition of calcite. The described deformation stage, reached under low tectonic stresses, followed a dilatant state characterized by increased porosity, pore size and permeability. At this stage pressure-solution was already a significant process of deformation.

引用

页码：565 / 575

页数：11

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