Late-stage diagenesis of illitic clay minerals as seen by decomposition of X-ray diffraction patterns: Contrasted behaviors of sedimentary basins with different burial histories

被引:33
作者
Lanson, B [1 ]
Velde, B
Meunier, A
机构
[1] Univ Grenoble, LGIT IRIGM, Environm Geochem Grp, F-38041 Grenoble 9, France
[2] Univ Grenoble, CNRS, F-38041 Grenoble, France
[3] Ecole Normale Super, CNRS, Geol Lab, F-75231 Paris 05, France
[4] Univ Poitiers, CNRS, Lab Petrol Alterat Hydrothermales, F-86022 Poitiers, France
关键词
clay minerals; decomposition; diagenesis; illite; illite-smectite; mixed layering; X-ray powder diffraction;
D O I
10.1346/CCMN.1998.0460108
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The smectite-to-illite diagenetic transformation has been documented in 5 different sedimentary basins using X-ray diffraction (XRD). Intermediate reaction products coexisting because of the effect of kinetics on this reaction have been characterized using decomposition of XRD patterns and comparison with calculated patterns. The nature and relative abundances of the various subpopulations of particles are shown to vary as a function of the geothermal gradient and of the age of the sediment. In all sedimentary basins that experienced a low steady geothermal gradient the physico-chemical characteristics (coherent scattering domain size [CSDS], junction probabilities) of intermediate mixed-layered illite-smectites (I-S) are similar. However, both the relative abundance and the crystallinity of the end-member illite increase as a function of the age of the sediment. In basins that have experienced a higher geothermal gradient, the CSDS of the I-S subpopulation is higher for a given illite content, indicating a slightly different reaction pathway. This difference in the characteristics (peak position and width) of elementary peaks may be used to infer the presence of such a high geothermal gradient when no other data are conclusive. In this case the growth of the illite end-member is favored over the growth of intermediate I-S phases even in young basins. Illitic phases formed from the alteration of kaolin minerals exhibit characteristics similar to the reaction products of the smectite-to-illite diagenetic transformation in the case of a high geothermal gradient. In contrast with what is observed in shale diagenesis, the characteristics of the illitic subpopulations describe a continuum with absolutely no gap in between subpopulations. In sandstone reservoirs, the various subpopulations crystallize simultaneously from a kaolin precursor. As a consequence, no kinship is expected between the various subpopulations.
引用
收藏
页码:69 / 78
页数:10
相关论文
共 37 条
[1]  
BOLES JR, 1979, J SEDIMENT PETROL, V49, P55
[2]  
Burst J.F., 1969, American Association of Petroleum Geologists Bulletin, V53, P73, DOI DOI 10.1306/5D25C595-16C1-11D7-8645000102C1865D
[3]  
EBERL DD, 1988, AM MINERAL, V73, P1335
[4]  
Francu J., 1989, GEOL CARPATH, V40, P355
[5]   VARIABILITY IN TEMPERATURE OF THE SMECTITE ILLITE REACTION IN GULF-COAST SEDIMENTS [J].
FREED, RL ;
PEACOR, DR .
CLAY MINERALS, 1989, 24 (02) :171-180
[6]   Clay mineral evolution in the Illinois Basin and its causes [J].
Gharrabi, M ;
Velde, B .
CLAY MINERALS, 1995, 30 (04) :353-364
[7]   SHALE DIAGENESIS IN THE BERGEN HIGH AREA, NORTH-SEA [J].
GLASMANN, JR ;
LARTER, S ;
BRIEDIS, NA ;
LUNDEGARD, PD .
CLAYS AND CLAY MINERALS, 1989, 37 (02) :97-112
[8]   ILLITE/SMECTITE DIAGENESIS AND ITS VARIABLE CORRELATION WITH VITRINITE REFLECTANCE IN THE PANNONIAN BASIN [J].
HILLIER, S ;
MATYAS, J ;
MATTER, A ;
VASSEUR, G .
CLAYS AND CLAY MINERALS, 1995, 43 (02) :174-183
[9]  
HOWER J, 1966, AM MINERAL, V51, P825
[10]  
HOWER J, 1976, GEOL SOC AM BULL, V87, P725, DOI 10.1130/0016-7606(1976)87<725:MOBMOA>2.0.CO