發(fā)布時(shí)間：2018-02-28 15:32

  本文關(guān)鍵詞： 地槽—地臺(tái)說(shuō) 板塊構(gòu)造 地球系統(tǒng)多圈層構(gòu)造觀 中—新生代 中國(guó)大地構(gòu)造　出處：《地質(zhì)論評(píng)》2017年05期 　論文類型：期刊論文

【摘要】：從19世紀(jì)中葉開始,大地構(gòu)造理論經(jīng)歷了從地槽—地臺(tái)說(shuō)到板塊構(gòu)造說(shuō)的發(fā)展過(guò)程。目前,板塊構(gòu)造說(shuō)雖然仍在盛行,但一個(gè)新的大地構(gòu)造理論——地球系統(tǒng)多圈層構(gòu)造觀(簡(jiǎn)稱多圈層構(gòu)造觀)已在形成中。地槽—地臺(tái)說(shuō),19世紀(jì)中葉提出,盛行于20世紀(jì)上半葉,是地質(zhì)學(xué)家從理論上研究地殼構(gòu)造及其演化的開始。地槽—地臺(tái)說(shuō)使用的方法是傳統(tǒng)的地質(zhì)學(xué)方法;研究領(lǐng)域是大陸地殼,褶皺帶(造山帶)和克拉通是其研究的核心內(nèi)容。地槽—地臺(tái)說(shuō)大大推動(dòng)了地質(zhì)科學(xué)的發(fā)展,并為地球科學(xué)的進(jìn)一步發(fā)展,奠定了良好的基礎(chǔ)。板塊構(gòu)造說(shuō),起始于20世紀(jì)60年代。板塊構(gòu)造使用的方法,除地質(zhì)學(xué)外,加上了地球物理學(xué)和地球化學(xué)等現(xiàn)代科學(xué)和技術(shù)手段;研究領(lǐng)域是全球大陸和海洋的巖石圈。板塊構(gòu)造說(shuō)使大地構(gòu)造學(xué)的研究范圍從地球表層擴(kuò)展到地球內(nèi)部,從大陸擴(kuò)展到海洋,極大地推動(dòng)了地球科學(xué)向更高的層次發(fā)展。目前,板塊構(gòu)造說(shuō)雖然仍在盛行,但是不足和缺陷已日益顯露出來(lái)。地球系統(tǒng)多圈層構(gòu)造觀,孕育于20世紀(jì)80年代晚期,目前正在發(fā)展中。地球系統(tǒng)多圈層構(gòu)造觀使用的方法更現(xiàn)代化,包括地質(zhì)學(xué)、地球物理學(xué)、地球化學(xué)以及一切探測(cè)地球深部和外層空間的方法、手段;研究領(lǐng)域,已不僅僅是地球表層的地殼或巖石圈,而是地球整體,地球各圈層的相互作用。我們相信,21世紀(jì)必將是地球系統(tǒng)多圈層構(gòu)造觀不斷發(fā)展、不斷完善的時(shí)代。中國(guó)及鄰區(qū)中、新生代構(gòu)造演化是全球研究多圈層構(gòu)造的最理想的切入點(diǎn)之一。我們期待中國(guó)地學(xué)工作者在新一輪大地構(gòu)造理論創(chuàng)新中發(fā)揮應(yīng)有的作用。
[Abstract]:Since the middle of 19th century, geotectonic theory has undergone the development from geosynclinic-platform to plate tectonics. But a new theory of geotectonics, the multi-ring tectonic view of the earth system, is in the process of being formed. The geosyncline-platform theory was put forward in the middle of the 19th century and prevailed in the first half of 20th century. It is the beginning of geologists' theoretical study of crustal structures and their evolution. The geosyncline-platform theory uses traditional geological methods; the field of study is the continental crust. Fold belt (orogenic belt) and craton are the core of its research. Geosyncline-platform theory has greatly promoted the development of geoscience and laid a good foundation for the further development of geoscience. Plate tectonics began in 1960s. In addition to geology, modern scientific and technical means such as geophysics and geochemistry were added to the plate tectonics. The field of study is the lithosphere of the global continent and ocean. Plate tectonics extends the study of geotectonics from the surface to the interior of the earth and from the continent to the ocean, which greatly promotes the development of geoscience to a higher level. Although the theory of plate tectonics is still prevailing, its shortcomings and defects have become increasingly apparent. The concept of multi-layer tectonics in the earth system was conceived in the late 1980s. More modern methods, including geology, geophysics, geochemistry, and all methods and means of detecting the deep and outer space of the Earth; research fields, It is not only the crust or lithosphere on the surface of the earth, but also the interaction of the earth as a whole and the various layers of the earth. We believe that the 21st century is bound to be an era of continuous development and improvement of the concept of multi-layer tectonics of the earth's system. Cenozoic tectonic evolution is one of the most ideal cut-in points for global research on multi-layer tectonics. We expect Chinese geoscientists to play their due role in the new round of tectonic theory innovation.
【作者單位】： 中國(guó)地質(zhì)科學(xué)院地質(zhì)研究所;
【基金】：中國(guó)地質(zhì)調(diào)查項(xiàng)目(編號(hào):DD20160343-01、DD20160343-02、12120115070301)的成果~~
【分類號(hào)】：P541

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