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| 1 | 超高压榴辉岩中金红石U-Pb年龄: 快速冷却的证据显示文摘对大别山南部超高压带内金河桥榴辉岩的金红石和绿辉石进行了U-Pb同位素分析, 利用等时线法和依据绿辉石Pb同位素组成扣除普通Pb法获得了一致的高精度金红石U-Pb年龄(218±1.2) Ma. 这表明低μ的绿辉石可以作为金红石普通Pb扣除的依据. 另外, 根据前人研究结果计算得到在快速冷却条件下金红石U-Pb体系封闭温度为(470±50)℃. 这一结果证明218 Ma代表超高压岩石冷却到470℃左右的时间, 而非峰期变质时代. 它证明大别山南部超高压岩石在峰期变质之后经历了一次快速冷却过程. | 李秋立 李曙光 周红英 李惠民 洪吉安 王清晨 H. -J. Massonne | 2001 | 科学通报2001，46，19： | 21 |
| 2 | 磷灰石中磁黄铁矿出溶结构的发现显示文摘中国东部苏鲁地区(江苏赣榆)出露大理岩-榴辉岩块体,其菱镁矿大理岩中保存的白云石分解结构表明地壳物质俯冲深度达到-200公里。在与该大理岩共生的榴辉岩中,我们发现了磷灰石的磁黄铁矿出溶结构。磷灰石是该榴辉岩的主要副矿物,其自形程度较高,与石榴石共生。样品中几乎所有磷灰石均发育出溶结构,至少存在两组相互垂直的出溶棒,它们各自严格沿同一个方向分布。出溶棒形状规则,宽度相近(<1μm),但长度变化大(5-50μm)。利用高分辨能谱仪测定其能谱,结果表明,出溶棒主要由Fe和S两种元素组成,但不能准确地确定其Fe/S比值。我们把这种出溶棒初步确定为磁黄铁矿(Fe1-xS)。磷灰石由于含大量稀土元素和挥发性组分如OH、F、Cl等以及我们所观察到的S,它的深循环因此可能对地球的水、硫以及其它挥发性组分的全球平衡具有重要影响。本文报道的磷灰石中磁黄铁矿出溶结构为深入探讨这个基本科学问题提供了一个新的突破口。 | 朱永峰 Massonne H J | 2005 | 岩石学报2005，21，2： | 18 |
| 3 | The effect of hydrogen bond acceptor properties of ionic liquids on their cellulose solubility显示文摘It is nowadays well-known that ionic liquids can dissolve cellulose. However, little systematic data has been published that shed light onto the influence of the ionic liquid structure on the dissolution of cellulose. We have conducted 1H NMR spectroscopy of ethanol in a large number of ionic liquids, and found an excellent correlation of the data obtained with the hydrogen acceptor properties (β-values). With this tool in hand, it is possible to distinguish between cellulose-dissolving and non-dissolving ionic liquids. A modulating effect of both, the anion of the non-dissolving ionic liquid and its cation was found in solubility studies with binary ionic liquid mixtures. The study was extended to other non-dissolving liquids, namely water and dimethylsulfoxide, and the effect of the cation was also investigated. | STARK Annegret SELLIN Martin ONDRUSCHKA Bernd MASSONNE Klemens | 2012 | Science China Chemistry2012，55，8： | 2 |
| 4 | Evidence for low-temperature ultrapotassic siliceous fluids in subduction zone environments from experiments in the system K2O-MgO-Al2O3-SiO2-H2O (KMASH) 显示文摘 | | 1991 | Lithos1991，28，： | 1 |
| 5 | Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite, and quartz显示文摘 | Massonne H J Schreyer W | 1987 | Contributions to Mineralogy and Petrology1987，96，： | 1 |
| 6 | Petrology of low-tempera- ture,ultrahigh-pressure marbles and interlayered eoesite ecle- gites near Sanqingge, Sulu terrane, eastern China显示文摘 | Zhu Y F Massonne H J Zhu M F | 2009 | Minera- logical Magazine2009，73，2： | 1 |
| 7 | Experimental high pressure investigation of partial melting in natural rocks and their influence on Vp and Vs 显示文摘 | Mueller H J Massonne H J | 2001 | Physics and Chemistry of the Earth(A)2001，26，45： | 1 |
| 8 | Experimental aspects of UHP metamorphism in pelitic systems 显示文摘 | | 1999 | International Geology Review1999，41，： | 1 |
| 9 | The low-high quartz and quartzcoesite transition to 40 kbar between 600℃ and 1600℃ and some reconnaissance data on the effect of NaAlO2 component on the low quartz-coesite transition显示文摘 | Mirwald P W Massonne H J | | 0，，12： | 1 |
| 10 | Thermodynamic properties of white micas on the basis of high-pressure experiments in the systems K2O- MgO-A1203-SiO2-H2O and K2O-FeO-Al2O3-SiO2-H2O 显示文摘 | Massonne H Szpurka Z | 1997 | Lithos1997，41，： | 1 |
| 11 | Biphasic acid scavenging utilizing ionic liquids:the first commercial process with ionic liquids 显示文摘 | Maase M Massonne K | 2005 | ACS Symposium Series2005，902，10： | 1 |
| 12 | Phase relations of siliceous marbles at ultrahigh pressure based on thermodynamic calculations: Examples from the Kokchetav Massif,Kazakhstan and the Sulu terrane, China 显示文摘 | Massonne H J | 2011 | Geological Journal2011，46，23： | 1 |
| 13 | Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite, and quartz显示文摘 | Hans -Joachim Massonne Werner Schreyer | 1987 | Contributions to Mineralogy and Petrology1987，，2： | 1 |
| 14 | Microdiamonds from the Saxonian Erzgebirge, Germany: In situ micro-Raman characterization 显示文摘 | Nasdala L Massonne H J | 2000 | European Journal of Mineralogy2000，12，2： | 1 |
| 15 | Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite, and quartz显示文摘 | Hans -Joachim Massonne Werner Schreyer | 1987 | Contributions to Mineralogy and Petrology1987，，2： | 1 |
| 16 | Metamorphic Evolution of Chloritoid-Bearing Micaschist from the Variscan Elstergebirge: Evidences for Stacking of High-Pressure Rocks in the Saxothuringian Zone of Central Europe显示文摘A chloritoid-garnet-bearing micaschist from the southern part of the Elstergebirge was studied to better understand the Variscan orogenic evolution in the Saxothuringian zone of the northwestern Bohemian Massif.Based on the textural relations and compositions of minerals,especially of zoned garnet and potassic white mica,a P-T path was reconstructed using contoured P-T pseudosections.The U-Th-Pb dating of monazite in the micaschist was undertaken with the electron microprobe.The micaschist experienced P-T conditions along a clockwise path between 16 kbar at 510℃and 5 kbar at 555℃followed by isobaric heating to about 600℃.Monazite ages range between 315 and 480 Ma with the most prominent maxima and side maxima at 346.0±1.1(2σ),357.3±2.3,and 368.3±1.7 Ma.Ages older than 380 Ma were related to detrital monazite pointing to a Devonian sedimentary protolith.Other ages around 325 Ma were assigned to the isobaric heating by nearby post-tectonic granites.The high-pressure event,being the result of the collision of Laurussia and Gondwana after closure of the Rheic Ocean,occurred in the Late Devonian.The exhumation to 15-20 km(5 kbar)ended probably in the Early Carboniferous.The high-pressure micaschists from the Fichtelgebirge to the Erzgebirge crystalline complexes are suggested to represent a single nappe within a metamorphic nappe pile.This nappe is composed of metasedimentary slices,which experienced different peak pressures rather than representing a coherent crustal section. | Gelareh Rahimi Hans-Joachim Massonne | 2020 | Journal of Earth Science2020，31，3： | 1 |
| 17 | Contribution to the Study of the Decomposition of SF6 in electric Arcs and Sparks显示文摘 | BECHER W MASSONNE J | 1970 | ETZ-A1970，91，1： | 1 |
| 18 | Evidence for low-temperature ultrapotassic siliceous fluids in subduction zone environments from experiments in the system K2O-MgO-Al2O3-SiO2-H2O (KMASH)显示文摘 | | 1992 | Lithos1992，28，： | 1 |
| 19 | Thermodynamic Roperties of White Micas on the Basis of High-Pressure Experi- ments in the Systems KzO-MgO-Al2 O3-H2 O and K2O- FeO-Al2O3-SiO2-H2O显示文摘 | MASSONNE H J SZPUEKA Z | 1997 | Lithos1997，41，13： | 1 |
| 20 | Thermodynamic properties of white micas on the basis of high-pressure exper/ments in the systems K20-MgO- Al2O3-SiO2-H2O and K2O-FeO-Al2O3-SiO2-H2O显示文摘 | Massonne H J Szpurka Z | 1997 | Lithos1997，41，： | 1 |
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