| 关于东南极拉斯曼丘陵夕线片麻岩类原岩恢复问题的讨论 |
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| 引用本文： | 任留东,耿元生,王彦斌,赵越.关于东南极拉斯曼丘陵夕线片麻岩类原岩恢复问题的讨论[J].地学前缘,2007,14(1):75-84. |
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| 作者姓名： | 任留东 耿元生 王彦斌 赵越 |
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| 作者单位： | 1. 中国地质科学院,地质研究所,北京,100037
2. 中国地质科学院,地质力学研究所,北京,100081 |
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| 基金项目： | 国家自然科学基金
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中国地质调查局区域地质调查项目
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国土资源部百名优秀青年科技人才计划 |
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| 摘 要： | 南极拉斯曼丘陵及其邻区的(含)夕线片麻岩类的原岩可以是杂砂岩、亚杂砂岩、石英砂岩、泥质岩或页岩等。粘土岩或页岩之类的富铝沉积岩与富夕线片麻岩并没有直接对应关系。没有一种泥质岩的化学组成可以与富夕线片麻岩相对应。研究区内夕线石片麻岩的形成主要与黑云斜长片麻岩有关,影响夕线石出现的决定性因素是特定温压条件下的变形变质改造过程,而不是原岩成分。夕线石片麻岩在很大程度上是黑云斜长片麻岩经长英质组分迁移之后的滞留-残留体。夕线石化过程中岩石组分发生了改造,相关变质作用已经明显偏离等化学过程,基本上属于开放体系。原岩中Al2O3的含量也不能控制夕线石的出现与否,含夕线石的岩石未必富铝,反之亦然,岩石富铝也可以不出现夕线石;但是夕线石化过程往往是Al2O3相对增加的过程,这些认识对于夕线石片麻岩成岩环境的确定和原岩建造的重建都具有重要意义。
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| 关 键 词： | 夕线片麻岩类 原岩恢复 铝含量 化学过程 南极拉斯曼丘陵 |
| 文章编号： | 1005-2321（2007）01-0075-10 |
| 收稿时间： | 2006-10-15 |
| 修稿时间： | 2006-12-16 |
On the protolith of the sillimanite gneisses in the Larsemann Hills,East Antarctica |
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| Ren Liudong,Geng Yuansheng,Wang Yanbin,Zhao Yue.On the protolith of the sillimanite gneisses in the Larsemann Hills,East Antarctica[J].Earth Science Frontiers,2007,14(1):75-84. |
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| Authors: | Ren Liudong Geng Yuansheng Wang Yanbin Zhao Yue |
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| Institution: | 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China 2. Institute of Geomechanics , Chinese Academy of Geological Sciences, Beijing 100081, China |
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| Abstract: | The protoliths of the sillimanite gneisses from the Larsemann Hills, east Antarctica, and their adjacent area may be greywacke, sub-greywacke, quartz sandstone, pelite or shale. The aluminum rich sediments such as clays or shale need not correspond to sillimanite-rich gneisses. No known argillaceous rock equals to sillirnanite-rich gneiss in chemical composition. The source rock from which the sillimanite gneisses derive is probably biotite plagioclase gneiss in the study area. It is the deformation-metamorphism process under pressure and temperature condition, not the original rock composition, that controls the presence of sillimanite. We suggest that the sillimanite gneiss is a mixture of materials from the migrating felsic melt, the biotite-plagioclase gneiss undergoing partial melting and the restites after the melt is removed. During metamorphism and sillirnanite formation the original rock changes its chemical composition and, the process is an open system, which deviates from being isochemical. In addition, the Al2O3 contents of the original rock is an important, but not critical factor for the formation of sillimanite, i. e. , the sillimanite-hearing rock need not be aluminum rich in composition, and vise versa, an aluminum-rich rock does not necessarily produce sillimanite. Therefore we postulate that the source rock from which the aluminum rich rocks derive need not be enriched in this ele- ment, but we point out that the formation of sillimanite generally involves a Alz03 increasing process. If correct, this conclusion is of significant implication for the determination of the sillimanite gneiss formation process and the reconstruction of the protolith setting. |
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| Keywords: | sillimanite gneiss protolith aluminum contents chemical process Larsemann Hills |
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