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Discussions on the mountains and orogenic belts and related issues
Hou QuanLin1; Guo QianQian1; Chen YiChao1; Cheng NanNan2; Shi MengYan2; Li JiLiang3
2021-08-01
Source PublicationACTA PETROLOGICA SINICA
ISSN1000-0569
Volume37Issue:8Pages:2287-2302
AbstractA good grasp of the distinctions between mountains and orogenic belts is crucial to the understanding of plate tectonics. The greatest innovation must be based on the inheritance of previous researches, therefore, this paper first reviews the research history from mountains to orogenic belts in Earth Science, and then concludes the distinctions between them, and lists some common questions in the study of orogenic belts. The research history of mountains, from morphology and the interpretation of uplifting to the internal structure, tectonics and the universal dynamics, follows the whole process of modern geology, from the birth to the geosyncline theory and finally the plate tectonics theory. The plate tectonics theory gives a more definite definition to orogenic belts and defines the tasks and objects of structural geology. As a topographic term, mountains only represent landmasses conspicuously above surroundings. The key point of mountains is the elevations and steep slops. They can be resulted from any horizontal stresses of extensional, compressional and shearing, or from vertical stresses governed by mantle plume or exoteric body impact. Orogen is a collective term and represents structures constructed by the collective work of convergent plate margin processes. Orogenic belts contain subductional and collisional orogenic belts. The key characteristics of orogenic belts are the subduction-controlled rock-structure associations. Orogenic belts emphasize the dynamic process while mountains emphasize the static form and the present morphology. Mountains and orogenic belts are two entirely different concepts. In the end, we outline some confused and misunderstood issues, as well as some unclear concepts, that remain to be discussed.
KeywordOrogenic belts Mountains Subduction metamorphism Melange Accretionary arc
DOI10.18654/1000-0569/2021.08.02
WOS KeywordCRUSTAL GROWTH ; TECTONICS ; EVOLUTION ; ARC
Language英语
WOS Research AreaGeology
WOS SubjectGeology
WOS IDWOS:000735639300003
PublisherSCIENCE PRESS
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/103946
Collection离退休科研人员
Corresponding AuthorHou QuanLin
Affiliation1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
2.Henan Polytech Univ, Sch Resources & Environm, Jiaozuo 454003, Henan, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
Recommended Citation
GB/T 7714
Hou QuanLin,Guo QianQian,Chen YiChao,et al. Discussions on the mountains and orogenic belts and related issues[J]. ACTA PETROLOGICA SINICA,2021,37(8):2287-2302.
APA Hou QuanLin,Guo QianQian,Chen YiChao,Cheng NanNan,Shi MengYan,&Li JiLiang.(2021).Discussions on the mountains and orogenic belts and related issues.ACTA PETROLOGICA SINICA,37(8),2287-2302.
MLA Hou QuanLin,et al."Discussions on the mountains and orogenic belts and related issues".ACTA PETROLOGICA SINICA 37.8(2021):2287-2302.
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