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Determination of pressure in aqueo-carbonic fluid inclusions at high temperatures from measured Raman frequency shifts of CO2
Yuan, Xueyin ; Mayanovic, Robert A. ; Zheng, Haifei ; Sun, Qiang
刊名AMERICAN MINERALOGIST
2017
关键词CO2 Raman spectroscopy pressure determination HDAC fluid inclusion DIAMOND-ANVIL CELL SPECTROSCOPIC CHARACTERIZATION GOLD MINERALIZATIONS SYSTEM H2O-CO2-NACL GRANITIC PEGMATITE PHASE-EQUILIBRIA FERMI RESONANCE ORE GENESIS SOUTH CHINA DENSITY
DOI10.2138/am-2017-5405
英文摘要Due to the presence of additional volatiles and/or electrolytes in CO2-H2O fluids, the total pressure of many natural aqueo-carbonic fluid inclusions at high temperatures as determined using microther-mometry is usually made with considerable uncertainty. In this paper, we present the results of our high P-T in situ Raman scattering study of high-density aqueo-carbonic fluids, with and without a small amount of CH4 and NaCl, whose objective is to derive a new method for pressure determination in aqueo-carbonic fluid inclusions at high temperatures. The measurement of the Fermi dyad bands at temperatures up to 400 degrees C and pressures up to 1200 MPa is described. The manner in which the frequency shifts and intensity of Raman bands are governed by pressure, temperature, presence of CH4 in carbonic and NaCl in aqueous fluids is discussed. From the monotonic dependence of the frequency shifts of the lower Fermi dyad band nu_ and the Fermi resonant splitting D (D = nu(+) - nu_) with pressure and temperature, the pressure (in MPa) in aqueo-carbonic fluid inclusions at elevated temperatures can be determined directly by using the following two polynomial equations: P (MPa) = -16 + 1.232x T -53.72x(Delta v_) 1.83 x 10(-3)x T-2 + 24.46x(Delta v_)(2) -0.292x Tx(Delta v_), P (MPa) = 26 + 1.501xT+ 193.24x(Delta D) 1.61 x 10(-3)xT(2)+ 5.436x(Delta D)(2) + 0.158xTx(Delta D), where T is in degrees C, Delta v_ and Delta D represent frequency shifts (in cm(-1)) of the lower band and the resonant splitting relative to the reference values measured at 23 degrees C and 6 MPa, respectively. Based on the attainable accuracy of the fitted peak positions and the results from fitting of Raman frequency shifts' dependence with pressure and temperature, the uncertainty in pressure determination is about 50 MPa for pressures determined from nu_ and 40 MPa from that determined from D.; National Natural Science Foundation of China [41373057]; China Scholarship Council [201406010059]; SCI(E); ARTICLE; 1-2; 404-411; 102
语种英语
内容类型期刊论文
源URL[http://ir.pku.edu.cn/handle/20.500.11897/476309]  
专题地球与空间科学学院
推荐引用方式
GB/T 7714
Yuan, Xueyin,Mayanovic, Robert A.,Zheng, Haifei,et al. Determination of pressure in aqueo-carbonic fluid inclusions at high temperatures from measured Raman frequency shifts of CO2[J]. AMERICAN MINERALOGIST,2017.
APA Yuan, Xueyin,Mayanovic, Robert A.,Zheng, Haifei,&Sun, Qiang.(2017).Determination of pressure in aqueo-carbonic fluid inclusions at high temperatures from measured Raman frequency shifts of CO2.AMERICAN MINERALOGIST.
MLA Yuan, Xueyin,et al."Determination of pressure in aqueo-carbonic fluid inclusions at high temperatures from measured Raman frequency shifts of CO2".AMERICAN MINERALOGIST (2017).
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