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Syntheses, single crystal structure analyses and ultraviolet light emission of CaW1-xMoxO4 (x= 0.0-1.0) scheelite-powellite solid solutions 白钨矿-粉晶固溶体CaW1-xMoxO4 (x= 0.0 ~ 1.0)的合成、单晶结构分析及紫外光发射
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.220901
K. Murai, K. Yamashita, Ginga Kitahara, M. Tokuda, A. Yoshiasa
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引用次数: 0
Identification of fracturing behavior in thermally cracked granite using the frequency spectral characteristics of acoustic emission 利用声发射频谱特征识别热裂花岗岩的破裂行为
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.221014
Kazumasa Sueyoshi, M. Kitamura, X. Lei, I. Katayama
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引用次数: 1
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 东南极洲Skallen l<s:1> zow- holm杂岩中石英-长石片麻岩中石榴石的化学分带和晶体尺寸分布:对地温学的意义
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.221129
T. Ikeda, Saori Goto
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引用次数: 0
Zircon geochronology of high-grade metamorphic rocks from outcrops along the Prince Olav Coast, East Antarctica: Implications for multi-thermal events and regional correlations 东南极洲王子奥拉夫海岸露头高品位变质岩的锆石年代学:多热事件和区域对比的意义
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.221220
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}
引用次数: 0
Zircon U-Pb ages of the Cretaceous gabbroic and granitic rocks from the Kajishima, northwest Shikoku, southwest Japan. 日本四国西北部鹿岛白垩系辉长岩和花岗质岩石的锆石U-Pb年龄
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.230224
Kazuya Shimooka, S. Saito, K. Tani
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引用次数: 0
Carbon dioxide and water in the crust. Part 1: equation of state for the fluid 地壳中的二氧化碳和水。第一部分:流体的状态方程
4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.221224a
Shumpei YOSHIMURA
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。
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引用次数: 0
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 东南极洲Dronning Maud地东部Prince Olav海岸Niban-nishi岩中含硅榴石-柘榴石泥质片麻岩的变质时代和压力-温度条件:托尼期变质作用的证据
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.221124
Y. Mori, T. Hokada, T. Miyamoto, T. Ikeda
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引用次数: 0
Kiryuite and gunmaite, two new minerals from Tsukubara, Kiryu City, Gunma Prefecture, Japan Kiryuite和gunmaite:日本群马县Kiryu市筑原的两种新矿物
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.230605
Daisuke NISHIO–HAMANE, Takeshi Yajima, Issei Ikari, Yoshiya Ohki, Hirofumi Hori, Yoshihiro Ohara
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引用次数: 0
Nd isotopic evolution of Archean tonalitic–granodioritic rocks of the Napier Complex, East Antarctica 东南极洲纳皮尔杂岩太古宙调性-花岗闪长岩的Nd同位素演化
4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.230330
Satoko SUZUKI, Tomokazu HOKADA, Masahiro ISHIKAWA, Takuji HAMAMOTO
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.
研究了东南极洲Napier杂岩中Riiser-Larsen山太古宙调性-花岗闪长正长岩体样品的Sm-Nd同位素。经SHRIMP锆石分析,原岩形成时的εNd≈0约为3.27 ~ 3.07 Ga。这与之前报道的Napier杂岩最古老调性正剖面的Sm-Nd全岩同位素数据不同,在3.87 ~ 3.80 Ga (TCHUR)显示εNd = 0,与SHRIMP锆石分析的约3.8 Ga一致。这些数据表明,体积大且均匀的调性花岗闪长岩在整个原岩变质过程中保持了εNd≈0的信号,岩石的源物质在约3.80、3.27和3.07 Ga时表现出εNd≈0的特征。纳皮尔杂岩的调性-花岗闪长岩正长岩可能包含古太古代至中太古代Nd同位素演化的遗传信息。
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引用次数: 0
Effect of acidic microbial polysaccharides on calcium carbonate polymorph formation in hot water at 40 - 80 oC 酸性微生物多糖对40 ~ 80℃热水中碳酸钙多晶形成的影响
IF 0.7 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.2465/jmps.221116
M. Kawano, Jinyeon Hwang
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引用次数: 0
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Journal of Mineralogical and Petrological Sciences
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