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Titlebook: Universals of Language Today; Sergio Scalise,Elisabetta Magni,Antonietta Bisetto Book 2009 Springer Science+Business Media B.V. 2009 Synta

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發(fā)表于 2025-3-21 19:21:51 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Universals of Language Today
編輯Sergio Scalise,Elisabetta Magni,Antonietta Bisetto
視頻videohttp://file.papertrans.cn/943/942250/942250.mp4
概述Includes a fresh and up-to-date survey of the present state of research on Universals of Language in an international context, with original contributions from leading specialists in the field.Feature
叢書名稱Studies in Natural Language and Linguistic Theory
圖書封面Titlebook: Universals of Language Today;  Sergio Scalise,Elisabetta Magni,Antonietta Bisetto Book 2009 Springer Science+Business Media B.V. 2009 Synta
描述This book collects the contributions presented at the international congress held at the University of Bologna in January 2007, where leading scholars of different persuasions and interests offered an up-to-date overview of the current status of the research on linguistic universals. The papers that make up the volume deal with both theoretical and empirical issues, and range over various domains, covering not only morphology and syntax, which were the major focus of Greenberg’s seminal work, but also phonology and semantics, as well as diachrony and second language acquisition. Diverse perspectives illustrate and discuss a huge number of phenomena from a wide variety of languages, not only exploring the way research on universals - tersects with different subareas of linguistics, but also contributing to the ongoing debate between functional and formal approaches to explaining the universals of language. This stimulating reading for scientists, researchers and postgraduate students in linguistics shows how different, but not irreconcilable, modes of explanation can complement each other, both offering fresh insights into the investigation of unity and diversity in languages, and p
出版日期Book 2009
關(guān)鍵詞Syntax; William Croft; future; language; morphology; phonology; semantics
版次1
doihttps://doi.org/10.1007/978-1-4020-8825-4
isbn_softcover978-90-481-7998-5
isbn_ebook978-1-4020-8825-4Series ISSN 0924-4670 Series E-ISSN 2215-0358
issn_series 0924-4670
copyrightSpringer Science+Business Media B.V. 2009
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 22:46:47 | 只看該作者
William Croftrade. It is a useful term for comparison of rocks within a single prograde metamorphic area. When applied to rocks in different regions, its meaning is not always clear, however, and its exact nature should be clearly specified.
板凳
發(fā)表于 2025-3-22 03:09:12 | 只看該作者
Elisabetta Magnied the following reaction for the formation of aluminum-rich chlorite:.Thus, as Correns remarked, in diagenesis some minerals are formed which also occur in metamorphism. “Therefore, we do not have a sharp boundary towards metamorphism.” This is certainly true, even if additional criteria are taken into account.
地板
發(fā)表于 2025-3-22 05:33:11 | 只看該作者
Geert Booij incorporated in granitic melts, and some of the reactions involving ferromagnesian minerals and melt will be discussed. Because of the lack of data obtained in synthetic systems, the discussion is based on results obtained from both natural and synthetic starting materials.
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發(fā)表于 2025-3-22 14:53:40 | 只看該作者
. An extensive bibliography, including the key contributions and classic papers in the field, make it an invaluable source book for graduate students and professional geologists..978-3-642-44234-6978-3-540-74169-5
7#
發(fā)表于 2025-3-22 19:45:16 | 只看該作者
0924-4670 tudents in linguistics shows how different, but not irreconcilable, modes of explanation can complement each other, both offering fresh insights into the investigation of unity and diversity in languages, and p978-90-481-7998-5978-1-4020-8825-4Series ISSN 0924-4670 Series E-ISSN 2215-0358
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發(fā)表于 2025-3-23 00:53:42 | 只看該作者
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發(fā)表于 2025-3-23 02:18:57 | 只看該作者
Emiliano Guevara,Sergio Scalisenot appear in the reaction equation, because H.O is always present in the fluid phase occurring in the rocks. In this chapter, reactions in rocks composed of quartz, dolomite, calcite o r magnesite are discussed, as they proceed in order of increasing temperature of metamorphism.
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發(fā)表于 2025-3-23 07:21:42 | 只看該作者
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