coesite
英['kəʊsaɪt]
美['koʊsaɪt]
- n. [矿]柯石英
双语例句
- 1. The coesite mainly changed quartz glomerocryst which made its including minerals creat radial cracks;
- 柯石英多已转化为石英聚晶，并使包裹它的矿物产生放射状胀裂纹；
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- 2. Coesite eclogite was discovered by the authors in Xinxian County, Henan Province, central China in 1992.
- 本文报道了一项中美合作研究的新进展：笔者于1992年在河南省新县发现了柯石英榴辉岩。
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- 3. Coesite (pseudomorph) inclusions is first discovered in hypostheny which reflect a well - developed radial cracks.
- 在紫苏辉石中首次发现柯石英假像的包体，显示清晰的放射状胀裂纹结构。
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- 4. The discovery of coesite -bearing eclogites in this area enlarges the region of coesite-bearing eclogite belt in Central -Eastern China.
- 河南大别山区含柯石英榴辉岩的发现扩大了中国中东部含柯石英榴辉岩带的分布区。
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- 5. As the important member in Dabie ultrahigh pressure metamorphic belt, meta-granitoids are often associated with coesite-bearing eclogites.
- 大别山超高压变质带中变质花岗岩常与榴辉岩密切伴生。
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- 6. Up to now there has been few studies on deformation of quartz in ultra-high rocks and quartz-coesite phase transition at differential stress.
- 目前对超高压岩石中石英的变形以及在差应力条件下石英-柯石英的相变研究程度低。
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- 7. Coesite has been first discovered in the eclogites and their country rocks -kyanite quartzite in the western area of Tuanma Fault from the Dabie Mountains, Henan province.
- 团麻断裂以西的河南大别山区榴辉岩及其围岩蓝晶石石英岩中首次发现柯石英。
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- 8. The notes describe the common minerals such as quartz and its polymorphs, coesite, tridymite and cristobalite, feldspar, plagioclase, feldspathoids, pyroxenes, amphiboles, etc.
- 讲稿详细地介绍了火成岩矿物，如：石英及它的同构异形体、柯石英、鳞石英、方石英、长石、斜长石、似长石、辉石、闪石等矿物。
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- 9. The hydrogen and oxygen isotope compositions of single minerals and whole-rock were measured for coesite-bearing eclogite at Shima and quartz-bearing eclogite at Huangzhen in southeastern Dabie.
- 本文报道了大别山东南部安徽石马地区柯石英榴辉岩组合和黄镇地区石英榴辉岩组合的全岩及单矿物的氢氧同位素特征。
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- 10. The hydrogen and oxygen isotope compositions of single minerals and whole-rock were measured for coesite-bearing eclogite at Shima and quartz-bearing eclogite at Huangzhen in southeastern Dabie.
- 本文报道了大别山东南部安徽石马地区柯石英榴辉岩组合和黄镇地区石英榴辉岩组合的全岩及单矿物的氢氧同位素特征。
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- Typical coesite pseudomorphs and SiO2 lamellae in omphacitic clinopyroxenes were hardly observed.
南带榴辉岩未见典型的柯石英假象，但绿辉石中也发现石英出溶片晶。
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