Magmatism and Crustal Evolution of the Tibetan Plateau
暫譯: 青藏高原的岩漿作用與地殼演化

這本書將非常獨特，因為目前沒有任何一本專注於西藏高原的岩漿與地殼演化的同類書籍。這本書將是第一本連貫且具主題性的出版物，將西藏高原的岩漿與地殼演化的所有方面整合在單一卷冊中。編寫這本關於地球上如此獨特地點的書籍，使得這本書在內容上也變得非常特別且獨特，未來許多年將成為備受追捧的出版物。這本書將包含大量新的地球化學、岩石學和地質年代學數據。這本書具有高度的跨學科性，整合了來自地球科學廣泛領域的多樣數據集、觀察結果和資訊。

Xuanxue Mo is an academician of the Chinese Academy of Science and a professor at China University of Geosciences. He has been at UC Berkeley and LBL Berkeley, USA for research (1981-1983). His research interests are igneous petrology, petrophysical chemistry, petrotectonics and mineralization, including (1) magmatism and tectonic evolution of the Tibetan Plateau and surrounding regions; (2) geodynamic background of mineralization and distribution of large - super large deposits in China, especially in the Tibetan Plateau and the southwest China; (3) experiments and modeling of phase equilibrium and thermodynamics of magma system. He has been teaching igneous and metamorphic petrology, thermodynamics of magmatic processes, and advanced Igneous petrology at both undergraduate and postgraduate levels.
Professor Jinfu Deng (1935-2021) was a professor at China University of Geosciences, Beijing. He had served the dean of the Department of Geology, the vice-chairman of theAcademic Committee of the University, the executive director of the Chinese Society of Mineralogy- Petrology-Geochemistry and so on. He was a visiting professor at the Department of Geology and Planetary Sciences at Caltech, USA (1986-1988). His research interests included igneous petrology, petrotectonics, petrophysical chemistry and mineralization. (1) He was the first to introduce physicochemistry into the study of genesis of igneous rocks, crust-mantle deep processes, regional petrogeotectonics and mineralization. (2) He proposed a theoretical model of 'continental roots-plume tectonics' on geodynamic evolution of lithosphere of China and Eurasia based on tectonic division at lithosphere scale and crust-mantle deep processes. (3) He proposed the composition profile and thermal structure model of the upper mantle in eastern China and revealed the huge thinning of the North China Craton lithosphere. (4) He proposed that the cataclysm of the lithosphere-asthenosphere system was the fundamental power source of the metallogenic "great explosion", which was efficiently applied to explaining metallogenic mechanism and evaluating mineral resources potential.
Zengqian Hou is an academician of the Chinese Academy of Science and a senior research geologist in Chinese Academy of Geological Sciences (CAGS) including served as the Director-General of Institute of Mineral Resources (2000-2005) and Institute of Geology (2005-2018), CAGS. He also serves as the Vice-President of NSFC (2018-2023), Chairman of the IGCP Committee of China (2016-2023) and Regional Vice President of the Society of Geology Applied to Mineral Deposits (2011-2013). He has conducted several major scientific projects including an IGCP project and two Chinese State Key 973 Fundamental Research Projects on the lithospheric architecture and relevant mineral systems in collisional orogenies. These researches have led to an establishment of a new theoretical framework and genetic models for collision-related metallogenesis (REE, Cu, Pb-Zn, Au), and major discoveries of world-class copper and other metallic deposits in China. He was thus awarded the Grand and First Prizes of National Scientific and Technical Advancement and Second Prize of National Natural Science. He also serves as and Regional Vice President of the Society of Geology Applied to Mineral Deposits (2011-2013).
Zhidan Zhao is a professor of petrology and geochemistry at China University of Geosciences in Beijing (CUGB). He received his BS (1990) and PhD (1995) degrees in Geochemistry at China University of Geosciences in Wuhan (CUGW). He completed postdoctoral research in the Institute of Geochemistry, Chinese Academy of Sciences in Guiyang in 1998 before joining the faculty at CUGB to date. In the intervening years, he was a visiting professor at UC Berkeley (2002-2003, 2012-2014) in collaboration with Professor Don DePaolo on isotopic geochemistry of postcollisional rocks from the Tibetan Plateau. He taught optical mineralogy, petrology, petrogeochemistry at both undergraduate and postgraduate levels. His research includes: (1) regional geochemistry on various rocks along the Qinling orogenic belts, (2) high pressure and high temperature experimental study of elastic wave velocity in rocks, and (3) petrology and geochemistry of the postcollisional magmatism on the Tibetan plateau and in the adjacent regions.
Guochen Dong is a professor at China University of Geosciences (Beijing). He has been both an educator and a researcher in Earth Science. He conducted geological mapping and mineral exploration in Hebei Geological Bureau (1983-1998) and taught optical mineralogy, mineralogy, petrology and field geology at both undergraduate and postgraduate levels in China University of Geosciences (2003-2023). His research includes: (1) petrology and geochemistry of granites and granitoid rocks and volcanic rocks related to the collision between Indian and Asia continentals; (2) magmatism associated with continental collision and continental crust accretion; (3) felsic and granitic rocks and related ore deposits; (4) genetic and prospecting mineralogy, geochronology and geological applications.
Di-Cheng Zhu is a professor of petrology and geochemistry at China University of Geosciences (Beijing) (CUGB), received his B.Sc. (1997) and M.Sc. (2000) from Chengdu University of Technology, China and Ph.D. (2003) from Chinese Academy of Geological Sciences, China. He joined the Chengdu Institute of Geology and Mineral Resources in 2003 and moved to CUGB in 2007 before became a professor in 2009. He devoted his enthusiasm to study the formation of the Tibetan Plateau from a magmatic perspective since 2000. His research interests include (1) magma generation and crustal evolution in collision zones, (2) magmatism and the formation of the Tibetan Plateau, and (3) paleogeographic reconstruction of microcontinents. He haspublished more than 180 research papers with total citations of more than 15000 times (Google Scholar h-index 59). He is currently serving as a Co-Editor-in-Chief of Lithos (2022-).
Yaoling Niu is currently an honorary professor at Laoshan Laboratory, China. He has been both an educator and a researcher in Earth Science. He taught crystallography, optical mineralogy, mineralogy, igneous and metamorphic petrology, elemental and isotope geochemistry, ore deposits, thermodynamics for geologists, global tectonics and field geology at both undergraduate and postgraduate levels in China (1982-1985), Australia (1993-2001), USA (1986-1987, 2003-2004) and UK (2005-2022). His research includes: (1) petrology and geochemistry of mantle peridotites, basalts and basaltic rocks, granites and granitoid rocks, high- and ultra-high-pressure metamorphic rocks and ore deposits; (2) ocean ridge magmatism, intraplate magmatism, subduction-zone processes, magmatism associated withcontinental collision and continental crust accretion; (3) causes and effects of seafloor subduction and global tectonics, chemical geodynamics and mantle circulation; (4) elemental and isotope geochemistry, geochronology and geological applications.

宣學默是中國科學院院士及中國地質大學的教授。他曾於1981年至1983年間在美國加州大學伯克利分校及伯克利國家實驗室進行研究。他的研究興趣包括火成岩岩石學、岩石物理化學、岩石構造學及礦化作用，具體包括：(1) 西藏高原及周邊地區的岩漿作用與構造演化；(2) 中國大型至超大型礦床的礦化背景及分佈，特別是在西藏高原及中國西南地區；(3) 岩漿系統的相平衡與熱力學的實驗與建模。他在本科及研究生階段教授火成岩及變質岩岩石學、岩漿過程的熱力學及高級火成岩岩石學。

鄭富登教授（1935-2021）是中國地質大學（北京）的教授。他曾擔任地質系主任、學校學術委員會副主席、中國礦物學-岩石學-地球化學學會執行理事等職位。他於1986年至1988年間擔任美國加州理工學院地質與行星科學系的訪問教授。他的研究興趣包括火成岩岩石學、岩石構造學、岩石物理化學及礦化作用。(1) 他是第一位將物理化學引入火成岩成因研究、地殼-地幔深部過程、區域岩石構造學及礦化作用的學者。(2) 他基於岩石圈尺度的構造劃分及地殼-地幔深部過程，提出了中國及歐亞大陸岩石圈地球動力學演化的“大陸根-熱柱構造”理論模型。(3) 他提出了中國東部上地幔的成分剖面及熱結構模型，揭示了華北克拉通岩石圈的巨大變薄。(4) 他提出岩石圈-軟流圈系統的劇變是金屬生成“巨大爆炸”的根本動力來源，並有效應用於解釋金屬生成機制及評估礦產資源潛力。

侯增乾是中國科學院院士及中國地質科學院的高級研究地質學家，曾擔任礦產資源研究所所長（2000-2005）及地質研究所所長（2005-2018）。他還擔任國家自然科學基金委員會副主席（2018-2023）、中國IGCP委員會主席（2016-2023）及應用於礦床地質學會的區域副主席（2011-2013）。他參與了多個重大科學項目，包括一個IGCP項目及兩個中國國家重點973基礎研究項目，研究碰撞造山帶的岩石圈結構及相關礦產系統。這些研究建立了與碰撞相關的金屬生成（稀土元素、銅、鉛鋅、金）新的理論框架及成因模型，並在中國發現了世界級的銅及其他金屬礦床。因此，他獲得了國家科技進步特等獎及一等獎和國家自然科學二等獎。

趙志丹是中國地質大學（北京）的岩石學及地球化學教授。他於1990年獲得中國地質大學（武漢）的學士學位，1995年獲得博士學位。他於1998年在中國科學院地球化學研究所完成博士後研究，隨後加入中國地質大學（北京）任教。此期間，他曾於2002-2003年及2012-2014年在加州大學伯克利分校擔任訪問教授，與Don DePaolo教授合作研究西藏高原後碰撞岩石的同位素地球化學。他教授光學礦物學、岩石學及岩石地球化學，涵蓋本科及研究生階段。他的研究包括：(1) 秦嶺造山帶各類岩石的區域地球化學；(2) 岩石中彈性波速的高壓高溫實驗研究；(3) 西藏高原及其周邊地區後碰撞岩漿作用的岩石學及地球化學。

董國臣是中國地質大學（北京）的教授。他在地球科學領域同時擔任教育者及研究者。他曾在河北省地質局進行地質測繪及礦產勘查（1983-1998），並在中國地質大學教授光學礦物學、礦物學、岩石學及野外地質學（2003-2023）。他的研究包括：(1) 與印度及亞洲大陸碰撞相關的花崗岩及花崗岩類岩石及火山岩的岩石學及地球化學；(2) 與大陸碰撞及大陸地殼增生相關的岩漿作用；(3) 酸性及花崗岩及相關礦床；(4) 成因及勘探礦物學、地球年代學及地質應用。

朱迪成是中國地質大學（北京）的岩石學及地球化學教授，於1997年獲得學士學位（成都理工大學），2000年獲得碩士學位，2003年獲得中國地質科學院博士學位。他於2003年加入成都地質礦產研究所，2007年轉至中國地質大學（北京），並於2009年成為教授。自2000年以來，他熱衷於從岩漿的角度研究西藏高原的形成。他的研究興趣包括：(1) 碰撞帶的岩漿生成及地殼演化；(2) 岩漿作用及西藏高原的形成；(3) 微陸塊的古地理重建。他已發表超過180篇研究論文，總引用次數超過15000次（Google Scholar h-index 59）。目前，他擔任《Lithos》的共同主編（2022-）。

牛耀靈目前是中國的榮譽教授，任職於青島的嶗山實驗室。他在地球科學領域同時擔任教育者及研究者。他曾在中國（1982-1985）、澳大利亞（1993-2001）、美國（1986-1987, 2003-2004）及英國（2005-2022）教授結晶學、光學礦物學、礦物學、火成及變質岩岩石學、元素及同位素地球化學、礦床、地質學熱力學、全球構造學及野外地質學。他的研究包括：(1) 地幔橄欖岩、玄武岩及玄武岩類岩石、花崗岩及花崗岩類岩石、高壓及超高壓變質岩及礦床的岩石學及地球化學；(2) 海洋脊岩漿作用、板內岩漿作用、隱沒帶過程、與大陸碰撞及大陸地殼增生相關的岩漿作用；(3) 海底隱沒及全球構造的成因與影響、化學地球動力學及地幔循環；(4) 元素及同位素地球化學、地球年代學及地質應用。