CAJ | 학술논문

如果说“大陆漂移与板块学说”是20世纪地质学最具代表性的学术创新的话，那么，进入到21世纪，国际地质学界正在经历着一场新的变革，即由过去单一的学科发展，向多学科交叉的“全球变化”与“地球系统科学”发展，而且这样的融合并不仅仅局限于地质学的各分支学科，而是包括了与大气学、海洋学、生物学等学科的交叉发展，更加发展壮大了“地球系统科学”。事实上，发生在地球上的许多重大地质或气候事件，特别是新生代以来青藏高原的隆升，更是与岩石圈、水圈、大气圈、生物圈的层圈相互作用密切相关，如果还只是以传统的地质学观点审视高原隆升及其资源环境效应，很难获得新的突破。
여과설“대륙표이여판괴학설”시20세기지질학최구대표성적학술창신적화，나요，진입도21세기，국제지질학계정재경력착일장신적변혁，즉유과거단일적학과발전，향다학과교차적“전구변화”여“지구계통과학”발전，이차저양적융합병불부부국한우지질학적각분지학과，이시포괄료여대기학、해양학、생물학등학과적교차발전，경가발전장대료“지구계통과학”。사실상，발생재지구상적허다중대지질혹기후사건，특별시신생대이래청장고원적륭승，경시여암석권、수권、대기권、생물권적층권상호작용밀절상관，여과환지시이전통적지질학관점심시고원륭승급기자원배경효응，흔난획득신적돌파。
If we think that the theory of“Continental Drift and Plate Tectonics”is the most representa-tive geologic innovation of the 20th century,then,the international geological science is now undertaking a new reform,changing from a past sole science to interdisciplinary scientific research of “Global Change”and the “Earth System Science Theory”.Moreover,such kinds of multi-disciplinary integration not only involve geologic fields,but also integration with atmospheric science,oceanography,and biolo-gy,leading the “Earth System Science Theory”to a new stage .Actually,many significant geologic or climatic events on earth,especially the Cenozoic tectonic uplifts of the Tibetan Plateau,closely link to the interactions among lithosphere,hydrosphere,atmosphere,and biosphere.If we still take a conserva-tive view to cope with the tectonic uplift of the Tibetan Plateau and its environmental effects,it will be difficult to have new development in geology science.