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Determination of pressure in aqueo-carbonic fluid inclusions at high temperatures from measured Raman frequency shifts of CO (sub 2)

Yuan Xueyin, Robert A. Mayanovic, Zheng Haifei and Sun Qiang
Determination of pressure in aqueo-carbonic fluid inclusions at high temperatures from measured Raman frequency shifts of CO (sub 2)
American Mineralogist (February 2017) 102 (2): 404-411

Abstract

Due to the presence of additional volatiles and/or electrolytes in CO (sub 2) -H (sub 2) O fluids, the total pressure of many natural aqueo-carbonic fluid inclusions at high temperatures as determined using microthermometry 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 CH (sub 4) 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 CH (sub 4) in carbonic and NaCl in aqueous fluids is discussed. From the monotonic dependence of the frequency shifts of the lower Fermi dyad band nu (sub -) and the Fermi resonant splitting D (D = nu (sub +) - nu (sub -) ) 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 + 1.232 X T - 53.72 X (Delta nu (sub -) ) - 1.83 X 10 (super -3) X T (super 2) +24.46 X (Delta nu (sub -) ) (super 2) - 0.292 X T X (Delta nu (sub -) ), P(MPa) = -26 + 1.501 X T + 193.24 X (Delta D) - 1.61 X 10 (super -3) X T (super 2) + 5.436 X (Delta D) (super 2) + 0.158 X T X (Delta D), where T is in degrees C, Delta nu (sub -) and Delta D represent frequency shifts (in cm (super -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 (sub -) and 40 MPa from that determined from D.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 102
Serial Issue: 2
Title: Determination of pressure in aqueo-carbonic fluid inclusions at high temperatures from measured Raman frequency shifts of CO (sub 2)
Affiliation: Peking University, Laboratory of Orogenic Belts and Crustal Evolution, Beijing, China
Pages: 404-411
Published: 201702
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
References: 56
Accession Number: 2017-018531
Categories: Geophysics of minerals and rocks
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 1 table
Secondary Affiliation: Missouri State University, USA, United States
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, copyright, Mineralogical Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201713
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