Tectono-magmatic evolution from accretion to collision in the southern margin of the Central Asian Orogenic Belt.
IF 1.7
3区 地球科学
Q2 GEOLOGY
引用次数: 0
中亚造山带南缘从增生到碰撞的构造-岩浆演化。
本文章由计算机程序翻译，如有差异，请以英文原文为准。
求助全文
约1分钟内获得全文
求助全文
来源期刊
岩石学报
Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
3.60
自引率
22.20%
发文量
5997
审稿时长
6 months
期刊介绍：
Acta Petrologica Sinica is an academic journal under the supervision of the Chinese Academy of Sciences and sponsored by the Chinese Society of Mineralogy, Petrology and Geochemistry and the Institute of Geology and Geophysics of the Chinese Academy of Sciences. The journal's publishing policy is to adhere to innovation, comprehensiveness, cutting-edge and orientation, advocate diversity and multi-school, rely on and unite the vast number of geoscientists across the country, explore the mysteries of nature, carry out extensive and in-depth basic theoretical research, promote the research and development of the field of earth science in my country, publish high-level scientific research results, and cultivate and train a large number of geoscientific research talents for my country.
Acta Petrologica Sinica mainly reports on various disciplines related to the basic theory of petrology, including important basic theories and applied research results in magmatic petrology, metamorphic petrology, sedimentary petrology, petrology geotectonics, rock isotope chronology and isotope geochemistry, rock mineralization, and rock-forming mineralogy. At the same time, the journal also publishes review articles, problem discussions, academic trends and book reviews.
求助内容：
应助结果提醒方式：
京公网安备 11010802042870号
