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和田河流域沙和基岩的角闪石成分及石英18O值
The Chemical Composition of Amphibole and Oxygen Composition of Quartz in Sands and Bedrocks in the Hotan River Basin
【摘要】 本文运用电子探针和氧同位素测试等手段,分析了和田河流域沙物质及某些有关基岩所含角闪石的种类、普通角闪石的化学成分和石英的δ18O值。沙物质和岩浆岩(钾长花岗岩)在所含角闪石种类以及普通角闪石化学成分上的差异性明显大于相似性,说明后者为前者提供的角闪石有限。另外,沙丘沙含有多种变质成因的角闪石。产生这种现象的合理解释是:变质岩风化产物是沙的重要物源。沙物质中石英δ18O值介于变质石英氧同位素成分范围,并且粒度愈细的石英,δ18O值愈高。根据基岩中云母片岩所含石英颗粒最细、δ18O值最高的特点判断,细沙物质在风扬过程中混入了较多的高δ18O值细粒变质石英。
【Abstract】 With EPMA and analysis of oxygen isotope composition, the typies of amphibole, chemical composition of hornblende and oxygen isotope composition of quartz in sands and bedrocks in the Hotan River basin were determined. There are a number of amphiboles developed in metamorphic rocks in sands, and the oxygen isotope compositions of quartz in dune sands and similar to that of metamorphic quartz. These cases are considered to results from the mixing of material dertived from metamorphic rocks.
【Key words】 sand; bedrock; chemical composition; oxygen isotope composition; material source.;
- 【文献出处】 干旱区研究 ,Arid Zone Research , 编辑部邮箱 ,1993年02期
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