浅析"龙江丝路带"地质旅游资源分布特征与构造作用
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摘要
利用GIS技术将"龙江丝路带"地质旅游资源分布与地貌、构造单元进行空间叠加,分析地质旅游资源的分布特征和成因,旨在为促进地方旅游业发展和科普宣传提供参考。111处地质旅游资源可划分为地貌景观、基础地质和地质灾害遗迹3大类,小兴安岭-千山隆起带、松辽沉降带的熔岩台地和低平原是资源最丰富的区带。古生代-中生代,华北、西伯利亚和西太平洋板块之间的构造运动是形成这种分布特征的主要地质营力。
The distribtion characteristics and causes of geological tourism resources in Longjiang Silk Road Zone were analyzed through the superposition of the spatial distribution,landform and tectonic units by GIS to provide references for promoting the development of local tourism and popular science propaganda. The result shows that in the study area,111 geological tourism resources could be summarized as landscape relics,basic geology relics and geological disasters relics systematically. And then,the lava platforms and low plains of the Xiao Hinggan Mountains-Qianshan Mountains uplift zone and Songliao subsidence zone are the areas with the richest geogical tourism resources. Further,from Paleozoic to Mesozoic,the tectonic activities between Northern China plate,Siberiain plate and Western Pacific plate had been the main geological forces for the formation of prensent distribution.
The distribtion characteristics and causes of geological tourism resources in Longjiang Silk Road Zone were analyzed through the superposition of the spatial distribution,landform and tectonic units by GIS to provide references for promoting the development of local tourism and popular science propaganda. The result shows that in the study area,111 geological tourism resources could be summarized as landscape relics,basic geology relics and geological disasters relics systematically. And then,the lava platforms and low plains of the Xiao Hinggan Mountains-Qianshan Mountains uplift zone and Songliao subsidence zone are the areas with the richest geogical tourism resources. Further,from Paleozoic to Mesozoic,the tectonic activities between Northern China plate,Siberiain plate and Western Pacific plate had been the main geological forces for the formation of prensent distribution.
引文
[1]冯天驷.地质旅游产业发展方向及其对策建议[J].中国地质矿产经济,1998(6):20-25.
[2]陈梦熊.加快开发我国的地质旅游资源[J].水文地质工程地质,2001(1):78.
[3]Hose T A. 3G's for modern geotourism[J]. Geoheritage,2012,4(1):7-24.
[4]Farsani N T,Coelho C,Costa C. Geotourism and geoparks sa novel strategies for socio-economic development in rural areas[J]. International Journal of Tourism-Research,2011,13(1):68-81.
[5]Newsome D,Dowling R K. The Scope and Nature of Geotourism[M]. Oxford:Elsvier Butterworth-Heinemann Ltd,2005:5-6.
[6]Megerle A. National geoparks and geotourism in Germany:framework and case study Baden-Wuerttemberg and Swabian Alb[J]. World Geoparks Newsl,2005(1):10-15.
[7]Boley B B,Nickerson N P,Bosak K. Measuring geotourism developing and testing the Geotraveler Tendency Scale(GTS)[J]. Journal of Travel Research,2011,50(5):567-578.
[8]Newsome D,Dowling R K. Natural Area Tourism:Ecology,Impacts and Management[M]. Bristol:Channel View Publications,2012:26-27.
[9]Miller N P. US National Parks and management of park soundscapes:A review[J]. Applied Acoustics,2008,69(2):77-92.
[10]Castaldini D,Valdati J,Ilies D C,et al. Geo-tourist map of the natural reserve of Salse di Nirano(Modena Apennines,northen Italy)[J].ⅡQuaternario,2005,18(1):245-255.
[11]郭威,丁华.论地质旅游资源[J].西安工程学院学报,2001,23(3):60-63.
[12]席岳婷,魏峰群.地质旅游资源保护与开发多元模式研究-以陕西黄河蛇曲地貌景观为例[J].西北大学学报(自然科学版),2006,36(4):643-647.
[13]王丽丽,马晓龙.基于规划文本分析的地质旅游资源价值演化研究-黄河石林案例[J].资源科学,2016,38(9):1653-1662.
[14]董静,郑天然,张雪梅.国家地质公园研究综述[J].石家庄学院学报,2006,8(6):86-92.
[15]曹养同,郭福生.地质公园的建设历程评述[J].国土与自然资源研究,2006(2):52-53.
[16]王雷,田明中,孙洪艳.中国山地型世界地质公园地质旅游的主要区域效益[J].山地学报,2015,33(6):733-741.
[17]Jones C. History of geoparks[J]. Geological Society,2008,300(1):273-277.
[18]向敬伟,李江风,王蕾,等.湖北长阳清江地质公园地质以及特征及地学意义[J].地球学报,2017,38(4):561-568.
[19]尹喜霖,张烽龙,单广杰.黑龙江省地质遗迹与自然保护区的开发保护[J].资源评价与保护,2003,20(3):29-31.
[20]钱丽萍,赵士德.基于地质遗迹的地质公园可持续发展模式研究-以五大连池世界地质公园为例[J].资源开发与市场,2006,22(6):557-560.
[21]缪瑞彬,肖寅妹,刘永顺,等.五大连池火山地质旅游资源特色研究[J].首都师范大学学报(自然科学版),2010,31(2):47-53.
[22]张洋,李文.黑龙江伊春小兴安岭国家地质公园地质遗迹资源评价与分级保护[J].东北林业大学学报,2016,44(4):98-101,106.
[23]王世进,万渝生,徐品,等.山东省地质公园的主要地质遗迹特征[J].地球学报,2015,36(5):669-684.
[24]Xiang Ye,Chen Jianqiang,Li Xuelin,et al. Development and utilization of geological tourism resources in Xiling Gorge of the Three Gorges[J]. Journal of Landscape Research,2011,3(2):64-68.
[25]段丽萍.西藏地质旅游资源概况及开发建议[J].地质通报,2006,25(1~2):302-307.
[26]何小芊,刘宇,熊国保.国内外地质旅游研究现状与展望[J].热带地理,2015,35(1):130-138.
[27]中国地质调查局.我国世界地质公园上升至33处[EB/OL]. http://www. cgs. gov. cn/xwl/ddyw/201603/t20160309_303425. html,2015-9-21.
[28]黑龙江省国土资源厅.黑龙江省地质公园概况[EB/OL]. http://www. hijlr. gov. cn/zwgk/zygk/dzhj/201610/t20161009_152917. html,2015-06-03.
[29]文立杰.镜泊湖[J].地质与资源,2014,26(s):74-75.
[30]陈铁男,张斌,杨文,等.嘉荫恐龙国家地质公园的建立及旅游资源的开发[J].国土资源科技管理,2003,20(6):42-44.
[31]赵济,陈永文,韩源丰.中国自然地理[M].北京:高等教育出版社,1995:20-40.
[32]蒋捷,杨昕.基于DEM中国地势三大阶梯定量划分[J].地理信息世界,2009(1):8-13.
[33]刘莹,吴朝阳,于世勇,等.辽宁省地质景观分布和地质旅游资源分区[J].国土与自然资源研究,2009(1):86-87.
[34]孙立新,张云,李影,等.内蒙古赤峰地区晚泥盆世双峰式火山岩地球化学特征与板内伸展事件[J].中国地质,2017,44(2):371-388.
[35]吴才来,陈安泽,高前明,等.东北伊春地区桃山古远古代花岗岩的发现[J].地质学报,2010,84(9):1324-1332.
[36]葛肖虹,马文璞.东北亚南区中-新生代大地构造轮廓[J].中国地质,2007,34(2):212-228.
[37]刘永江,张兴洲,金巍,等.东北地区晚古生代区域构造演化[J].中国地质,2010,37(4):943-951.
[38]朱群,刘斌,柴璐,等.东北亚南部地区地质与矿产-暨东北亚地区地质矿产综合图件编制[M].北京:地质大学出版社,2014:45-100.
[39]葛荣峰,张庆龙,王良书,等.松辽盆地构造演化与中国东部构造体质转换[J].地质论评,2010,56(2):180-195.
[2]陈梦熊.加快开发我国的地质旅游资源[J].水文地质工程地质,2001(1):78.
[3]Hose T A. 3G's for modern geotourism[J]. Geoheritage,2012,4(1):7-24.
[4]Farsani N T,Coelho C,Costa C. Geotourism and geoparks sa novel strategies for socio-economic development in rural areas[J]. International Journal of Tourism-Research,2011,13(1):68-81.
[5]Newsome D,Dowling R K. The Scope and Nature of Geotourism[M]. Oxford:Elsvier Butterworth-Heinemann Ltd,2005:5-6.
[6]Megerle A. National geoparks and geotourism in Germany:framework and case study Baden-Wuerttemberg and Swabian Alb[J]. World Geoparks Newsl,2005(1):10-15.
[7]Boley B B,Nickerson N P,Bosak K. Measuring geotourism developing and testing the Geotraveler Tendency Scale(GTS)[J]. Journal of Travel Research,2011,50(5):567-578.
[8]Newsome D,Dowling R K. Natural Area Tourism:Ecology,Impacts and Management[M]. Bristol:Channel View Publications,2012:26-27.
[9]Miller N P. US National Parks and management of park soundscapes:A review[J]. Applied Acoustics,2008,69(2):77-92.
[10]Castaldini D,Valdati J,Ilies D C,et al. Geo-tourist map of the natural reserve of Salse di Nirano(Modena Apennines,northen Italy)[J].ⅡQuaternario,2005,18(1):245-255.
[11]郭威,丁华.论地质旅游资源[J].西安工程学院学报,2001,23(3):60-63.
[12]席岳婷,魏峰群.地质旅游资源保护与开发多元模式研究-以陕西黄河蛇曲地貌景观为例[J].西北大学学报(自然科学版),2006,36(4):643-647.
[13]王丽丽,马晓龙.基于规划文本分析的地质旅游资源价值演化研究-黄河石林案例[J].资源科学,2016,38(9):1653-1662.
[14]董静,郑天然,张雪梅.国家地质公园研究综述[J].石家庄学院学报,2006,8(6):86-92.
[15]曹养同,郭福生.地质公园的建设历程评述[J].国土与自然资源研究,2006(2):52-53.
[16]王雷,田明中,孙洪艳.中国山地型世界地质公园地质旅游的主要区域效益[J].山地学报,2015,33(6):733-741.
[17]Jones C. History of geoparks[J]. Geological Society,2008,300(1):273-277.
[18]向敬伟,李江风,王蕾,等.湖北长阳清江地质公园地质以及特征及地学意义[J].地球学报,2017,38(4):561-568.
[19]尹喜霖,张烽龙,单广杰.黑龙江省地质遗迹与自然保护区的开发保护[J].资源评价与保护,2003,20(3):29-31.
[20]钱丽萍,赵士德.基于地质遗迹的地质公园可持续发展模式研究-以五大连池世界地质公园为例[J].资源开发与市场,2006,22(6):557-560.
[21]缪瑞彬,肖寅妹,刘永顺,等.五大连池火山地质旅游资源特色研究[J].首都师范大学学报(自然科学版),2010,31(2):47-53.
[22]张洋,李文.黑龙江伊春小兴安岭国家地质公园地质遗迹资源评价与分级保护[J].东北林业大学学报,2016,44(4):98-101,106.
[23]王世进,万渝生,徐品,等.山东省地质公园的主要地质遗迹特征[J].地球学报,2015,36(5):669-684.
[24]Xiang Ye,Chen Jianqiang,Li Xuelin,et al. Development and utilization of geological tourism resources in Xiling Gorge of the Three Gorges[J]. Journal of Landscape Research,2011,3(2):64-68.
[25]段丽萍.西藏地质旅游资源概况及开发建议[J].地质通报,2006,25(1~2):302-307.
[26]何小芊,刘宇,熊国保.国内外地质旅游研究现状与展望[J].热带地理,2015,35(1):130-138.
[27]中国地质调查局.我国世界地质公园上升至33处[EB/OL]. http://www. cgs. gov. cn/xwl/ddyw/201603/t20160309_303425. html,2015-9-21.
[28]黑龙江省国土资源厅.黑龙江省地质公园概况[EB/OL]. http://www. hijlr. gov. cn/zwgk/zygk/dzhj/201610/t20161009_152917. html,2015-06-03.
[29]文立杰.镜泊湖[J].地质与资源,2014,26(s):74-75.
[30]陈铁男,张斌,杨文,等.嘉荫恐龙国家地质公园的建立及旅游资源的开发[J].国土资源科技管理,2003,20(6):42-44.
[31]赵济,陈永文,韩源丰.中国自然地理[M].北京:高等教育出版社,1995:20-40.
[32]蒋捷,杨昕.基于DEM中国地势三大阶梯定量划分[J].地理信息世界,2009(1):8-13.
[33]刘莹,吴朝阳,于世勇,等.辽宁省地质景观分布和地质旅游资源分区[J].国土与自然资源研究,2009(1):86-87.
[34]孙立新,张云,李影,等.内蒙古赤峰地区晚泥盆世双峰式火山岩地球化学特征与板内伸展事件[J].中国地质,2017,44(2):371-388.
[35]吴才来,陈安泽,高前明,等.东北伊春地区桃山古远古代花岗岩的发现[J].地质学报,2010,84(9):1324-1332.
[36]葛肖虹,马文璞.东北亚南区中-新生代大地构造轮廓[J].中国地质,2007,34(2):212-228.
[37]刘永江,张兴洲,金巍,等.东北地区晚古生代区域构造演化[J].中国地质,2010,37(4):943-951.
[38]朱群,刘斌,柴璐,等.东北亚南部地区地质与矿产-暨东北亚地区地质矿产综合图件编制[M].北京:地质大学出版社,2014:45-100.
[39]葛荣峰,张庆龙,王良书,等.松辽盆地构造演化与中国东部构造体质转换[J].地质论评,2010,56(2):180-195.