K. Murai, K. Yamashita, Ginga Kitahara, M. Tokuda, A. Yoshiasa
{"title":"Syntheses, single crystal structure analyses and ultraviolet light emission of CaW1-xMoxO4 (x= 0.0-1.0) scheelite-powellite solid solutions","authors":"K. Murai, K. Yamashita, Ginga Kitahara, M. Tokuda, A. Yoshiasa","doi":"10.2465/jmps.220901","DOIUrl":"https://doi.org/10.2465/jmps.220901","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68832458","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Kazumasa Sueyoshi, M. Kitamura, X. Lei, I. Katayama
{"title":"Identification of fracturing behavior in thermally cracked granite using the frequency spectral characteristics of acoustic emission","authors":"Kazumasa Sueyoshi, M. Kitamura, X. Lei, I. Katayama","doi":"10.2465/jmps.221014","DOIUrl":"https://doi.org/10.2465/jmps.221014","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68832509","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Chemical zoning and crystal size distribution of garnet in a quartzo-feldspathic gneiss from the Lützow-Holm Complex at Skallen, East Antarctica: Implication for geothermometry","authors":"T. Ikeda, Saori Goto","doi":"10.2465/jmps.221129","DOIUrl":"https://doi.org/10.2465/jmps.221129","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68832872","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Ippei Kitano, T. Hokada, S. Baba, A. Kamei, Y. Motoyoshi, Prayath Nantasin, N. Setiawan, Davaa-ochir Dashbaatar, T. Toyoshima, M. Ishikawa, T. Katori, N. Nakano, Y. Osanai
{"title":"Zircon geochronology of high-grade metamorphic rocks from outcrops along the Prince Olav Coast, East Antarctica: Implications for multi-thermal events and regional correlations","authors":"Ippei Kitano, T. Hokada, S. Baba, A. Kamei, Y. Motoyoshi, Prayath Nantasin, N. Setiawan, Davaa-ochir Dashbaatar, T. Toyoshima, M. Ishikawa, T. Katori, N. Nakano, Y. Osanai","doi":"10.2465/jmps.221220","DOIUrl":"https://doi.org/10.2465/jmps.221220","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68833058","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Zircon U-Pb ages of the Cretaceous gabbroic and granitic rocks from the Kajishima, northwest Shikoku, southwest Japan.","authors":"Kazuya Shimooka, S. Saito, K. Tani","doi":"10.2465/jmps.230224","DOIUrl":"https://doi.org/10.2465/jmps.230224","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68833412","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
H2O–CO2-dominated fluids play a crucial role in most geological phenomena involving fluid–mineral–melt interactions. The equation of state is an essential tool for understanding the phenomena because it predicts the thermodynamic properties of the fluids. The modified Lee–Kesler equation of state for H2O–CO2 mixture fluid developed by Duan and Zhang (2006) is the most accurate at present and is applicable to a wide pressure–temperature range (∼ 2573 K and ∼ 10 GPa). Because of its high accuracy and wide applicable range, the equation has been used for constructing solubility laws in silicate melts. In this paper I review the Duan and Zhang (2006) equation of state and present the calculation procedure. Because the equation for calculating the partial fugacity coefficient is erroneously presented in the original paper, the correct equation is provided here. A C-language code and a Windows executable program for computing thermodynamic properties are provided for the convenience of users. The influence of the nonideal behaviour of the H2O–CO2 mixture fluid on some geological situations is discussed.
在大多数涉及流体-矿物-熔体相互作用的地质现象中,以h2o - co2为主的流体起着至关重要的作用。状态方程是理解这些现象的重要工具,因为它预测了流体的热力学性质。Duan和Zhang(2006)提出的修正的H2O-CO2混合流体Lee-Kesler状态方程是目前最精确的,适用于较宽的压力-温度范围(~ 2573 K和~ 10 GPa)。该方程精度高,适用范围广,可用于构造硅酸盐熔体中的溶解度规律。本文回顾了Duan and Zhang(2006)的状态方程,并给出了计算过程。由于原文中给出的部分逸度系数计算公式有误,本文给出了正确的计算公式。为了方便用户,提供了计算热力学性质的c语言代码和Windows可执行程序。讨论了H2O-CO2混合流体的非理想性质对某些地质情况的影响。
{"title":"Carbon dioxide and water in the crust. Part 1: equation of state for the fluid","authors":"Shumpei YOSHIMURA","doi":"10.2465/jmps.221224a","DOIUrl":"https://doi.org/10.2465/jmps.221224a","url":null,"abstract":"H2O–CO2-dominated fluids play a crucial role in most geological phenomena involving fluid–mineral–melt interactions. The equation of state is an essential tool for understanding the phenomena because it predicts the thermodynamic properties of the fluids. The modified Lee–Kesler equation of state for H2O–CO2 mixture fluid developed by Duan and Zhang (2006) is the most accurate at present and is applicable to a wide pressure–temperature range (∼ 2573 K and ∼ 10 GPa). Because of its high accuracy and wide applicable range, the equation has been used for constructing solubility laws in silicate melts. In this paper I review the Duan and Zhang (2006) equation of state and present the calculation procedure. Because the equation for calculating the partial fugacity coefficient is erroneously presented in the original paper, the correct equation is provided here. A C-language code and a Windows executable program for computing thermodynamic properties are provided for the convenience of users. The influence of the nonideal behaviour of the H2O–CO2 mixture fluid on some geological situations is discussed.","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135911234","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Metamorphic age and pressure–temperature conditions recorded in a sillimanite-garnet-bearing pelitic gneiss from Niban-nishi Rock of Niban Rock on the Prince Olav Coast, eastern Dronning Maud Land, East Antarctica: Evidence for Tonian metamorphism","authors":"Y. Mori, T. Hokada, T. Miyamoto, T. Ikeda","doi":"10.2465/jmps.221124","DOIUrl":"https://doi.org/10.2465/jmps.221124","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68832734","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Kiryuite and gunmaite, two new minerals from Tsukubara, Kiryu City, Gunma Prefecture, Japan","authors":"Daisuke NISHIO–HAMANE, Takeshi Yajima, Issei Ikari, Yoshiya Ohki, Hirofumi Hori, Yoshihiro Ohara","doi":"10.2465/jmps.230605","DOIUrl":"https://doi.org/10.2465/jmps.230605","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68833695","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
We examined Sm–Nd isotopes of samples from the Archean tonalitic–granodioritic orthogneiss mass of Mt. Riiser-Larsen in the Napier Complex, East Antarctica. Analytical data show εNd ≈ 0 of ca. 3.27 and ca. 3.07 Ga at the time of protolith formation, as determined by SHRIMP zircon analyses. This differs from previously reported Sm–Nd whole-rock isotope data from the oldest tonalitic orthogneisses of Mt. Sones in the Napier Complex, which show εNd = 0 at 3.87 to 3.80 Ga (TCHUR), which is coincident with ca. 3.8 Ga from SHRIMP zircon analyses. These data suggest that the voluminous and homogeneous tonalitic–granodioritic rocks retained the εNd ≈ 0 signal throughout the protolith–metamorphic process and that the source materials of the rocks showed εNd ≈ 0 at ca. 3.80, 3.27 and 3.07 Ga. Tonalitic–granodioritic orthogneisses from the Napier Complex may contain genetic information regarding Nd isotopic evolution from the Paleoarchean to Mesoarchean.
{"title":"Nd isotopic evolution of Archean tonalitic–granodioritic rocks of the Napier Complex, East Antarctica","authors":"Satoko SUZUKI, Tomokazu HOKADA, Masahiro ISHIKAWA, Takuji HAMAMOTO","doi":"10.2465/jmps.230330","DOIUrl":"https://doi.org/10.2465/jmps.230330","url":null,"abstract":"We examined Sm–Nd isotopes of samples from the Archean tonalitic–granodioritic orthogneiss mass of Mt. Riiser-Larsen in the Napier Complex, East Antarctica. Analytical data show εNd ≈ 0 of ca. 3.27 and ca. 3.07 Ga at the time of protolith formation, as determined by SHRIMP zircon analyses. This differs from previously reported Sm–Nd whole-rock isotope data from the oldest tonalitic orthogneisses of Mt. Sones in the Napier Complex, which show εNd = 0 at 3.87 to 3.80 Ga (TCHUR), which is coincident with ca. 3.8 Ga from SHRIMP zircon analyses. These data suggest that the voluminous and homogeneous tonalitic–granodioritic rocks retained the εNd ≈ 0 signal throughout the protolith–metamorphic process and that the source materials of the rocks showed εNd ≈ 0 at ca. 3.80, 3.27 and 3.07 Ga. Tonalitic–granodioritic orthogneisses from the Napier Complex may contain genetic information regarding Nd isotopic evolution from the Paleoarchean to Mesoarchean.","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135158543","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Effect of acidic microbial polysaccharides on calcium carbonate polymorph formation in hot water at 40 - 80 oC","authors":"M. Kawano, Jinyeon Hwang","doi":"10.2465/jmps.221116","DOIUrl":"https://doi.org/10.2465/jmps.221116","url":null,"abstract":"","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.7,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68832613","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}