气候变化领域集成服务门户(CCPortal): The interdependence of deformational and thermal processes in mountain belts

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DOI	10.1126/science.273.5275.637
	The interdependence of deformational and thermal processes in mountain belts
	Huerta A.D.; Royden L.H.; Hodges K.V.
发表日期	1996
ISSN	0036-8075
起始页码	637
结束页码	639
卷号	273 期号:5275
英文摘要	Crustal temperatures within collisional orogens are anomalously high compared with temperatures at comparable depths in stable continents, which is evidence of thermal processes that are fundamental to orogenesis. These temperatures can be explained by the redistribution of crust enriched in heat-producing elements through the accretion of crust from the down-going plate to the upper plate and surface erosion. With the use of geologically reasonable rates, the model results predict high temperatures (over 600°C) and inverted upper-plate geotherms (about 100°C over 20 kilometers) at shallow depths (20 to 40 kilometers) by 25 to 35 million years after collision. This study emphasizes the interdependence of deformational, surficial, and thermal processes.
英文关键词	geology; geometry; priority journal; review; temperature; thermodynamics; continental collision; deformation; heat producing element; orogenesis; thermal processes
语种	英语
来源期刊	Science
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/244092
作者单位	Dept. Earth, Atmosph., Planet. Sci., Massachusetts Inst. of Technology, Cambridge, MA 02139, United States
推荐引用方式 GB/T 7714	Huerta A.D.,Royden L.H.,Hodges K.V.. The interdependence of deformational and thermal processes in mountain belts[J],1996,273(5275).
APA	Huerta A.D.,Royden L.H.,&Hodges K.V..(1996).The interdependence of deformational and thermal processes in mountain belts.Science,273(5275).
MLA	Huerta A.D.,et al."The interdependence of deformational and thermal processes in mountain belts".Science 273.5275(1996).