Experimental growth of quartz in petroleum environment. Part I: Procedures and fluid trapping

被引:28
作者
Teinturier, S [1 ]
Pironon, J [1 ]
机构
[1] UHP, CREGU, UMR G2R, F-54506 Vandoeuvre Les Nancy, France
关键词
D O I
10.1016/j.gca.2003.11.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The quartz-water-oil-gas system has been experimentally studied with the objective of investigating the trapping of petroleum and aqueous inclusions in quartz at different water/oil (W/O) ratios (0/100, 5/95, 10/90, 20/80, 50/50, 100/0). Experiments were carried out in both a gas-pressure autoclave (GPA) under CH, pressure control, up to 250degreesC and 212 bar, and in a fluid-pressure autoclave (FPA) up to 350degreesC and 400 bar. High p-T conditions have notably allowed the growth of quartz at high oil saturation levels (W/O ratios from 10/90 to 50/50). Petroleum inclusions have been synthesised inside quartz microfractures (W/O ratios from 0/100 to 50/50; 209-350degreesC; 175-400 bar), and also inside quartz overgrowths (W/O ratios from 10/90 to 50/50; 289-350degreesC; 350-400 bar). Aqueous inclusions have been synthesised in presence of oil inside quartz microfractures from 185degreesC-163 bar up to 400degreesC-400 bar, and inside quartz overgrowth from 277degreesC-330 bar. Synthesised petroleum inclusions are representative of the parent oil up to 250degreesC. At 350degreesC, evidence of a cracking process has been observed with the consequent formation of methane. The segregation of the oil/gas/water column inside the GPA autoclave may also have prevented methane diffusion into the water phase when oil is present. This experimental approach shows that the trapping of fluid inclusions and the formation of quartz cement, under conditions of high oil saturation, have not been suppressed or prevented. Copyright (C) 2004 Elsevier Ltd.
引用
收藏
页码:2495 / 2507
页数:13
相关论文
共 58 条
[1]  
ANTHONY TR, 1974, N GEOL SOC, V1, P313
[2]   Combined use of Confocal Laser Scanning Microscopy and PVT simulation for estimating the composition and physical properties of petroleum in fluid inclusions [J].
Aplin, AC ;
Macleod, G ;
Larter, SR ;
Pedersen, KS ;
Sorensen, H ;
Booth, T .
MARINE AND PETROLEUM GEOLOGY, 1999, 16 (02) :97-110
[3]  
BARCLAY SA, 2000, INT ASS SEDIMENTOLOG, V29, P103
[4]   SYNTHETIC FLUID INCLUSIONS IN NATURAL QUARTZ .3. DETERMINATION OF PHASE-EQUILIBRIUM PROPERTIES IN THE SYSTEM H2O-NACL TO 1000-DEGREES-C AND 1500 BARS [J].
BODNAR, RJ ;
BURNHAM, CW ;
STERNER, SM .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1985, 49 (09) :1861-1873
[5]  
BROWN PE, 1989, AM MINERAL, V74, P1390
[6]   TIMING DIAGENESIS IN THE TARTAN RESERVOIR (UK NORTH-SEA) - CONSTRAINTS FROM COMBINED CATHODOLUMINESCENCE MICROSCOPY AND FLUID INCLUSION STUDIES [J].
BURLEY, SD ;
MULLIS, J ;
MATTER, A .
MARINE AND PETROLEUM GEOLOGY, 1989, 6 (02) :98-&
[7]   Characterization of water in synthetic rhyolitic glasses and natural melt inclusions by Raman spectroscopy [J].
Chabiron, A ;
Pironon, J ;
Massare, D .
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2004, 146 (04) :485-492
[8]  
DIXON SA, 1989, AAPG BULL, V73, P707
[9]   AN EQUATION OF STATE FOR THE CH4-CO2-H2O SYSTEM .1. PURE SYSTEMS FROM 0-DEGREES-C TO 1000-DEGREES-C AND 0 TO 8000 BAR [J].
DUAN, ZH ;
MOLLER, N ;
WEARE, JH .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1992, 56 (07) :2605-2617
[10]   Determination of chlorinity in aqueous fluids using Raman spectroscopy of the stretching band of water at room temperature: Application to fluid inclusions [J].
Dubessy, J ;
Lhomme, T ;
Boiron, MC ;
Rull, F .
APPLIED SPECTROSCOPY, 2002, 56 (01) :99-106