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Hydrous Carbonatitic Liquids Drive CO 2 Recycling From Subducted Marls and Limestones 含水碳酸盐岩液体推动俯冲泥灰岩和灰岩的co2再循环
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch18
Erwin Schettino, S. Poli
Pelagic limestones are subducted in a variety of subduction zones worldwide. Despite the geochemical relevance of systems enriched in CaCO3, previous experimental investigations mostly focused on carbonated pelites, with low Ca/(Ca+Mg+Fe) ratio. We present the compositions and the formation conditions of liquids in the model system CaO‐Al2O3‐SiO2‐H2O‐CO2 (CASHC), building on phase relationships in the subsystems CHC and CSHC, where a second critical endpoint was suggested at temperatures as low as 515 °C, and 3.2 GPa. Multianvil experiments were performed at 4.2 and 6.0 GPa on five bulk compositions at variable Ca/Si/Al ratios. H2O contents vary from 5.6 to 21 wt%. Aragonite + kyanite + vapor and minor lawsonite form at 700 °C, replaced by zoisite/grossular at 800 °C. Between 850 °C and 950 °C, a complex sequence of textural features is observed upon quenching of a single volatile‐rich liquid phase formed at run conditions. Precipitates include dendritic CaCO3, silicate glass, and Al‐rich whiskers. The bulk composition of such hydrous carbonatitic liquids is retrieved by image analysis on X‐ray maps, showing Ca/Si ratio increasing with pressure and temperature. Hydrous Ca‐carbonatitic liquids are efficient media for scavenging volatiles from subducted crustal material and for metasomatizing the mantle wedge. 18
远洋灰岩在世界范围内的各种俯冲带中都有俯冲。尽管富含CaCO3的体系具有地球化学意义,但以往的实验研究主要集中在低Ca/(Ca+Mg+Fe)比的碳酸化泥质体上。基于CHC和CSHC两个子系统的相关系,我们提出了CaO - Al2O3 - SiO2 - H2O - CO2 (CASHC)模型系统中液体的组成和形成条件,其中第二个临界端点建议在低至515°C和3.2 GPa的温度下。在4.2和6.0 GPa下,对不同Ca/Si/Al比例的五种体成分进行了多砧实验。水的含量从5.6%到21%不等。700℃时形成文石+蓝晶石+蒸汽石和少量的钙辉石,800℃时为黝帘石/钠辉石。在850°C和950°C之间,在运行条件下形成的单一富含挥发性的液相淬火时,观察到复杂的结构特征序列。析出物包括树枝状CaCO3、硅酸盐玻璃和富铝晶须。通过对X射线图的图像分析,获得了这种含水碳酸盐岩液体的总体组成,显示Ca/Si比随着压力和温度的增加而增加。含水Ca - carbonatitic液体是从俯冲的地壳物质中清除挥发物和使地幔楔交代的有效介质。18
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引用次数: 10
Predicted Speciation of Carbon in Subduction Zone Fluids 俯冲带流体中碳的预测形态
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch24
M. Guild, E. Shock
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引用次数: 4
Pressure‐Induced sp 2 ‐ sp 3 Transitions in Carbon‐Bearing Phases 含碳相压力诱导的sp - 2 - sp - 3转变
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch1
S. Lobanov, A. Goncharov
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引用次数: 1
The Effect of Variable Na/K on the CO 2 Content of Slab‐Derived Rhyolitic Melts 变Na/K对板坯流纹岩熔体CO 2含量的影响
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch17
Michelle Muth, Megan S. Duncan, R. Dasgupta
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引用次数: 4
Experimental Determination of Calcite Solubility in H 2 O‐KCl‐NaCl‐LiCl Solutions at 700°C and 8 kbar 方解石在h2o - KCl - NaCl - LiCl溶液中700°C和8kbar溶解度的实验测定
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.CH21
J. Eguchi
Understanding the interactions between calcite and aqueous solutions is important when studying the deep carbon cycle. The present study investigates the solubility of calcite in salt-H2O fluids at 700 °C and 8 kbar. The investigated salts included NaCl, KCl, LiCl, and CsCl. All experiments were conducted in a piston cylinder apparatus. The results show that calcite solubility increases with increasing concentration of any individual salt. The data were successfully fit to simple functions of the square of salt mole fraction. At a given salt concentration, the solubility enhancement increases with decreasing salt cation size. Experiments in the fluids with mixtures of multiples of salts were used to derive simple relations that can be used to predict calcite solubility in a wide range of salt solutions at the studied conditions. The results provide a basis for extending this approach to different pressures, temperatures, and salt compositions.
在研究深层碳循环时,了解方解石和水溶液之间的相互作用是很重要的。本研究考察了方解石在700°C和8kbar的盐- h2o流体中的溶解度。研究的盐类包括NaCl、KCl、LiCl和CsCl。所有的实验都是在活塞缸装置中进行的。结果表明,方解石溶解度随盐浓度的增加而增加。数据成功地拟合为盐摩尔分数平方的简单函数。在一定的盐浓度下,随着盐阳离子尺寸的减小,溶解度增强增大。在多种盐混合的流体中进行实验,得出了简单的关系式,可用于预测在所研究条件下方解石在各种盐溶液中的溶解度。结果为将该方法扩展到不同的压力、温度和盐成分提供了基础。
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引用次数: 1
Phase and Melting Relations of Fe 3 C to 300 GPa and Carbon in the Core 铁3c - 300 GPa与芯内碳的物相及熔化关系
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch3
Suguru Takahashi, E. Ohtani, T. Sakai, S. Kamada, S. Ozawa, T. Sakamaki, M. Miyahara, Yoshinori Ito, N. Hirao, Y. Ohishi
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引用次数: 5
Phase Diagrams of Carbonate Materials at High Pressures, with Implications for Melting and Carbon Cycling in the Deep Earth 碳酸盐材料在高压下的相图,及其对地球深部熔融和碳循环的影响
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch14
K. Litasov, A. Shatskiy, I. Podborodnikov, A. Arefiev
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引用次数: 6
High‐Pressure Carbonaceous Phases as Minerals 作为矿物的高压碳质相
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch2
O. Tschauner
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引用次数: 0
Carbon Redox Chemistry 碳氧化还原化学
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch7
C. Yoo
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引用次数: 0
Mixed Fluids of Water and Carbon Dioxide 水和二氧化碳的混合液体
Pub Date : 2020-03-24 DOI: 10.1002/9781119508229.ch20
E. Abramson
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引用次数: 0
期刊
Geophysical monograph
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