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高压超高压变泥质岩适用的地质温压计评述
引用本文:王晓赛,杜瑾雪,田野.高压超高压变泥质岩适用的地质温压计评述[J].岩石矿物学杂志,2018,37(2):325-341.
作者姓名:王晓赛  杜瑾雪  田野
作者单位:中国地质大学(北京)地球科学与资源学院;地质出版社;
基金项目:国家自然科学基金项目(41502059);中央高校基本业务费专项资金项目(2652015041)
摘    要:高压超高压变泥质岩形成温压条件及p-T演化轨迹是高压超高压变质作用研究的重要内容。本文介绍了高压超高压变泥质岩适用的几种地质温压计,包括石榴子石-多硅白云母Fe~(2+)-Mg交换温度计、石榴子石-绿泥石Fe~(2+)-Mg交换温度计、硬绿泥石-绿泥石Fe~(2+)-Mg交换温度计、多硅白云母Si含量压力计、金红石Zr含量温度计、榍石Zr含量温压计、锆石Ti含量温度计、石英Ti含量温度计以及氧同位素温度计,并对上述温压计的适用条件及使用时的注意事项做了简要评述。

关 键 词:高压超高压变泥质岩  常量元素温压计  微量元素温压计  氧同位素温度计
收稿时间:2017/2/20 0:00:00

Review on geothermobarometers for (ultra)high-pressure metapelites
WANG Xiao-sai,DU Jin-xue and TIAN Ye.Review on geothermobarometers for (ultra)high-pressure metapelites[J].Acta Petrologica Et Mineralogica,2018,37(2):325-341.
Authors:WANG Xiao-sai  DU Jin-xue and TIAN Ye
Institution:School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China,School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China and Geological Publishing House, Beijing 100083, China
Abstract:p-T conditions and p-T paths of (ultra)high-pressure metapelites are important aspects in the study of (ultra)high-pressure metamorphism. This paper introduces several kinds of geothermobarometers applicable to (ultra)high-pressure metapelites, which include the garnet-phengite Fe2 + -Mg exchange geothermometer, garnet-chlorite Fe2 + -Mg exchange geothermometer, chloritoid-chlorite Fe2 + -Mg exchange geothermometer, Si-in-phengite geobarometer, Zr-in-rutile geothermometer, Zr-in-titanite geothermobarometer, Ti-in-zircon geothermobarometer, Ti-in-quartz geothermobarometer and oxygen isotope geothermometer. In addition, a review is given concerning the applicable conditions and points for attention in use of the above geothermobarometers.
Keywords:(ultra)high-pressure metapelites  major element geothermometer  trace element geothermobarometer  oxygen isotope geothermometer
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