太白山核心自然景观及其成景作用研究
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摘要
指出了太白山是秦岭造山带的主要山脉,具有重要和特殊的景观类型。通过实地考察和对太白山综合研究,根据景观特征的差异性和特殊性,提出了太白山核心自然景观主要划分为冰川遗迹景观、山地景观、植被景观和气象景观,并对其特征、分布、成因进行了系统性阐述,认为太白山成景作用主要与太白山花岗岩岩体、新构造运动、气候环境及第四纪冰川四大因子密切相关。此结果可为太白山整体科学研究、旅游资源利用与保护提供了阶段性进展和依据。
Taibai mountain is main mountain range of Qinlingorogenic belt with significant and typical landscape types.Through field investigation and comprehensive study of Taibai mountain.,the main and key landscapes are the glacier landscape,mountain landscape,vegetation landscape and meteorological landscape.The characteristics,distribution and mechanism of Taibai are systematically expounded.It is systematically expounded that the role of Taibai Mountain is closely related to the Taibaishan granite body,neotectonic movement,climatic environment and Quaternary glaciers.The results can provide a staged progress and basis for the overall scientific research and tourism resource utilization and protection of Taibai Mountain.
Taibai mountain is main mountain range of Qinlingorogenic belt with significant and typical landscape types.Through field investigation and comprehensive study of Taibai mountain.,the main and key landscapes are the glacier landscape,mountain landscape,vegetation landscape and meteorological landscape.The characteristics,distribution and mechanism of Taibai are systematically expounded.It is systematically expounded that the role of Taibai Mountain is closely related to the Taibaishan granite body,neotectonic movement,climatic environment and Quaternary glaciers.The results can provide a staged progress and basis for the overall scientific research and tourism resource utilization and protection of Taibai Mountain.
引文
[1]齐矗华,甘枝茂,惠振德,等.太白山及其邻近地区冰川地貌的基本特征[J],陕西师大学报(自科版),1985(4):53~69.
[2]康永祥,刘婧辉,孙菲菲,等.太白山高山林线区太白红杉林年轮宽度对气候变化的响应[J].东北林业大学报,2010,38(8):11~13.
[3]张威,刘锐,魏亚刚,等.秦岭太白山冰缘地貌特征与环境[J].干旱区资源与环境,2016,30(10):171~178.
[4]傅志军.太白山气象风景旅游资源的开发利用[J].陕西师范大学学报(自科版),1999(s1):147~149.
[5]万红莲.太白山森林公园生态旅游资源初步调查[J].宝鸡文理学院学报(自科版),2006,26(2):162~164.
[6]田泽生.太白山第四纪冰川遗迹的探讨[J].西北大学学报(自然科学版),1981(3):59~69.
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[8]戴君虎,崔海亭,唐志尧,等.太白山高山带环境特征[J].山地学报,2001,19(4):299~305.
[9]宋雅琼,罗耀,李双成,等.太白山三清池湖泊沉积记录的全新世气候变化及周期讨论[J].湖泊科学,2016,28(4):899~908.
[10]党维华,郝杨,杨苗苗.太白山生态旅游区开发现状与旅游可持续发展探讨[J].西北林学院学报,2010,25(5):220~223.
[11]徐煜坚.中国第四纪冰川遗迹的初步考察[J].第四纪研究,1989(3):249~253.
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[13]翟丹平,白红英,秦进,等.秦岭太白山气温直减率时空差异性研究[J].地理学报,2016,71(9):1587~1595.
[14]吕星球,王晓霞,柯昌辉,等.北秦岭太白花岗岩体LA-ICPMS锆石U-Pb测年及其地质意义[J].矿床地质,2014,33(1):37~52.
[15]方小敏.青藏高原隆升阶段性[J].科技导报,2017,35(6):42~50.
[16]葛永刚,魏明建.青藏高原隆升综合研究[J].首都师范大学学报(自然科学版),2004,25(S1):128~136.
[17]郭进京,韩文峰,李雪峰.西秦岭新生代以来地质构造过程对青藏高原隆升和变形的约束[J].地学前缘,2009,16(6):215~225.
[18]李智超,李文厚,李永项,等.渭河盆地新生代沉积相研究[J].古地理学报,2015,17(4):529~540.
[19]张威,刘亮,刘啸,等.秦岭“太白冰期”冰坎宇宙成因核素10Be定年[J].科学通报,2014,59(31):3086~3094.
[2]康永祥,刘婧辉,孙菲菲,等.太白山高山林线区太白红杉林年轮宽度对气候变化的响应[J].东北林业大学报,2010,38(8):11~13.
[3]张威,刘锐,魏亚刚,等.秦岭太白山冰缘地貌特征与环境[J].干旱区资源与环境,2016,30(10):171~178.
[4]傅志军.太白山气象风景旅游资源的开发利用[J].陕西师范大学学报(自科版),1999(s1):147~149.
[5]万红莲.太白山森林公园生态旅游资源初步调查[J].宝鸡文理学院学报(自科版),2006,26(2):162~164.
[6]田泽生.太白山第四纪冰川遗迹的探讨[J].西北大学学报(自然科学版),1981(3):59~69.
[7]穆艳,张景群.太白山森林公园主要林型林内景观的定量评价[J].西北农林科技大学学报(自然科学版),2008,36(6):119~125.
[8]戴君虎,崔海亭,唐志尧,等.太白山高山带环境特征[J].山地学报,2001,19(4):299~305.
[9]宋雅琼,罗耀,李双成,等.太白山三清池湖泊沉积记录的全新世气候变化及周期讨论[J].湖泊科学,2016,28(4):899~908.
[10]党维华,郝杨,杨苗苗.太白山生态旅游区开发现状与旅游可持续发展探讨[J].西北林学院学报,2010,25(5):220~223.
[11]徐煜坚.中国第四纪冰川遗迹的初步考察[J].第四纪研究,1989(3):249~253.
[12]Molnar P,Boos W R,Battisti D S.Orographic controls on climate and paleoclimate of Asia:Thermal and mechanical roles for the Tibetan Plateau[J].Annual Review of Earth and Planetary Sciences,2010,38(1):77~102.
[13]翟丹平,白红英,秦进,等.秦岭太白山气温直减率时空差异性研究[J].地理学报,2016,71(9):1587~1595.
[14]吕星球,王晓霞,柯昌辉,等.北秦岭太白花岗岩体LA-ICPMS锆石U-Pb测年及其地质意义[J].矿床地质,2014,33(1):37~52.
[15]方小敏.青藏高原隆升阶段性[J].科技导报,2017,35(6):42~50.
[16]葛永刚,魏明建.青藏高原隆升综合研究[J].首都师范大学学报(自然科学版),2004,25(S1):128~136.
[17]郭进京,韩文峰,李雪峰.西秦岭新生代以来地质构造过程对青藏高原隆升和变形的约束[J].地学前缘,2009,16(6):215~225.
[18]李智超,李文厚,李永项,等.渭河盆地新生代沉积相研究[J].古地理学报,2015,17(4):529~540.
[19]张威,刘亮,刘啸,等.秦岭“太白冰期”冰坎宇宙成因核素10Be定年[J].科学通报,2014,59(31):3086~3094.