流体包裹体各相体积测定的现状和探索

doi:10.11867/j.issn.1001-8166.1995.06.0555

地球科学进展 ›› 1995, Vol. 10 ›› Issue (6): 555 -561. doi: 10.11867/j.issn.1001-8166.1995.06.0555

流体包裹体各相体积测定的现状和探索

常兆山

北京大学地质系 100871

收稿日期:1994-05-16 修回日期:1994-11-03 出版日期:1995-12-01
通讯作者: 常兆山

VOLUM EMEASUREMENT OF INDIVIDUAL PHASES IN A INCLUSION:PRESENT STATUS AND ADVANCES

Chang Zhaoshan

Department of Geology, Peking University, Beijing 100871

Received:1994-05-16 Revised:1994-11-03 Online:1995-12-01 Published:1995-12-01

下载PDF ( 723 )

流体包裹体研究是地质研究的重要手段之一，而流体包裹体各相的体积则是一个重要的参数。早期得不到体积数据，只能给出包裹体的二维面积。中国科学院地球化学研究所包裹体实验室曾提出一条换算曲线，根据二维面积推测体积，误差较大。Bodnar曾提出根据气泡直径和流体P-V-T-X性质计算包裹体体积的方法，本文对其未考虑到的情况进行了补充。还提出了根据实验资料用图解得到包裹体各相体积的新方法，并据实例比较了各种方法的优缺点。

关键词: 流体包裹体, 体积测定, Bodnar方法补充, 图解法

Fluid inclusion research is one of the important aspects of geology study, and the volumes of individual phases in a inclusion are significant parameters. In early time, only the two-dimension area on the focus plane could be measured. A curve was proposed to estimate the volume of inclusion based on the two-dimension area, but the error is large. Bodnar suggested to calculate the volume of individual phase based on the diameter of the vaper bubble and the P-V-T-X properties of the fluid, and his method is supplemented in this paper for uncovered situation. A new method using figures obtained from experimental data is put forward here. Finally, an example is presented and methods mentioned above are compared.

Key words: Fluid inclusion, Volume measurement, Supplement to Bodnar’s method, Method using figures.

[1] Roedder E. 流体包裹体.长沙:中南工业大学出版社，1984.
[2] 何知礼.包体矿物学.北京:地质出版社，1982.
[3] 季荣伦，陶谋镇等.矿物中包裹体的物理化学状态变量P-V-T-N之间的关系以及包裹体测温中应注意的问题. 矿物中包裹体研究.北京:科学出版社，1981.
[4] 卢焕章，李秉伦等.包裹体地球化学.北京:科学出版社，1990.
[5] 徐九华.H₂O-NaCl-CO₂体系液相状态方程及其在热液矿床研究中的应用.地球化学，1991，(3).
[6] Roedder E. Fluid inclusions as sample of ore fluids. In: Barnes H L eds. Geochemistry of Hydrothermal Ore Deposits. New York: Holt Rinehert and Winston Inc，1967.
[7] Roedder E and Skinner B J. Experimental evidence that fluid inclusions do not leak.Economic Geology，1968，63.
[8] Roedder E.Fluid inclusions studies on the porphyry-type oredeposits of Bingham，Utah，Butte，Montana and Climax，Colorado. Economic Geology，1971，66.
[9] Burrus R C. Analysis of fluid inclusions:phase equilibria at constant volume. American Journal of Science，1981，281.
[10] Ishkov Y M and Reyf F G. Laser spectral analysis of the liquid in individual inclusions. Geochemistry International，1980，17.
[11] Kelly W C and Rye R Q. Geologic fluid inclusion and stable isotope studies of the tin-tungsten deposits of Panasqueira，Portugal. Economic Geology，1979，74.
[12] Bodnar J D. A method of calculating fluid inclusion volumes based on vaper bubble diameters and P-V-T-X properties of fluid. Economic Geology，1983，78.
[13] Potter R W II，Babcock R S and Brown D L. A new method for determining the solubility of salts in aqueous solutions at elevated temperatures.US Geol Servey Jour Research，1977，5.
[14] Potter R W II，Clynne M A and Brown D L. Freezing point depression of aqueous sodium chloride solutions. Economic Geology，1978，73.
[15] Sankins F J. High copper content of fluid inclusions in quartz from northern Sonora: Implications for ore genesis theory. Geology，1952，9.
[16] Bowers T S and Heigeson H C. Calculation of the thermodynamic and geochemical sequences of nonideal mixing in the systemH₂O-CO₂-NaCl on phase relations in geologic systems:equition of state for H₂O-CO₂-NaCl fluids at high pressures and temperatures. Geochimica et Cosmochimica Acta，1983，47.
[17] Kavalieris I，Walshe J L and Harrold B P. Dome-related gold mineralization in the Pani Volcanic Complex，North Sulawesi，Indonesia: A study of geologic relations，fluid inclusions，and chlorite compositions. Economic Geology，1990，85.

[1]	张为,周丽,唐红峰,李和平,王力. 水热体系中 Na₂SO₄/K₂SO₄ 溶解度的热力学计算[J]. 地球科学进展, 2019, 34(4): 414-423.
[2]	王九一, 刘成林. 石盐流体包裹体中古嗜盐菌的研究进展[J]. 地球科学进展, 2016, 31(12): 1220-1227.
[3]	曹青，赵靖舟，赵小会，张涛，王宝清. 鄂尔多斯盆地宜川—黄陵地区马家沟组流体包裹体特征及其意义[J]. 地球科学进展, 2013, 28(7): 819-828.
[4]	孙贺,肖益林. 流体包裹体研究：进展、地质应用及展望[J]. 地球科学进展, 2009, 24(10): 1105-1121.
[5]	刘兴起;倪培. 表生环境条件形成的石盐流体包裹体研究进展[J]. 地球科学进展, 2005, 20(8): 856-862.
[6]	郑海飞;段体玉;孙樯;乔二伟. 一种潜在的地质压力计：流体包裹体子矿物的激光拉曼光谱测压法[J]. 地球科学进展, 2005, 20(7): 804-808.
[7]	李兆丽;胡瑞忠;彭建堂;毕献武;李晓敏. 稀有气体同位素示踪成矿古流体研究进展[J]. 地球科学进展, 2005, 20(1): 57-063.
[8]	赵靖舟. 油气成藏年代学研究进展及发展趋势[J]. 地球科学进展, 2002, 17(3): 378-383.
[9]	秦朝建，裘愉卓. 岩浆（型）碳酸岩研究进展[J]. 地球科学进展, 2001, 16(4): 501-507.
[10]	孙青,曾贻善. 单个流体包裹体成分无损分析进展[J]. 地球科学进展, 2000, 15(6): 673-678.

阅读次数

全文

摘要