[1]Kim S S,Wong K K F,Cho M.Assessing the economic value of a world heritage site and willingness-to-pay determinants:A case of Changdeok Palace[J].Tourism Management,2007,28(1):317-322.[2]Haynes D,Muller J,Carter S.Pesticide and herbicide residues in sediments and sea grasses from the Great Barrier Reef World Heritage area and Queensland Coast[J].Marine Pollution Bulletin,2000,41(7-12):279-287.[3]Paina D J,Sanchezb A,Meharg A A.The Donana ecological disaster:Contamination of a world heritage estuarine marsh ecosystem with acidified pyritemine waste[J].The Science of the Total Environment,1998,222(1-2):45-54.[4]Zoppi U,Barbetti M,Fletcher R,et al.The contribution of 14C AMS dating to the Greater Angkor archaeological project[J].Nuclear Instruments and Methods in Physics Research (Section B:Beam Interactions with Materials and Atoms),2004,223/224:681-685.[5]Maikhuri R K,Nautiyal S,Rao K S,et al.Conservation policy-people conflicts:A case study from Nanda Devi Biosphere Reserve (a World Heritage Site) India[J].Forest Policy and Economics,2001,2(3-4):355-365.[6]Kucukkaya A G.Photogrammetry and remote sensing in archeology[J].Journal of Quantitaqtive Spectroscopy and Radiative Transfer,2004,88(1-3):83-88.[7]Steinberg F.Conservation and rehabilitation of Urban Heritage in developing countries[J].Habitat International,1996,20(3):463-475.[8]Kingsford R T.Development strains on Australias greatest desert river system Cooper Greek[J/OL].IPAA National Conference,2001.http://www.nsw.ipaa.org.au /00-pdfs/paper7.pdf 2007.[9]葛云健,杨桂山,张忍顺,等.江苏沿海辐射沙洲申报世界自然遗产预研究[J].南京师范大学报(自然科学版),2009,32(3):125-129.[10]向岚麟.近22年世界遗产地研究进展——基于13种中文期刊的考察[J].旅游学刊,2009,24(4):85-88.[11]吴月,范坤,李陇堂.阿拉善腾格里沙漠地质公园旅游资源及其综合评价[J].中国沙漠,2009,29(3):409-414.[12]郑本兴,张林源,胡孝宏.玉门关西雅丹地貌的分布和特征及形成时代问题[J].中国沙漠,2002,22(1):40-46.[13]穆斯塔法·哈里默夫,福里茨·弗兹尔.中央亚细亚的八种雅丹地貌类型[J].中国沙漠,1990,10(1):1-11.[14]杨更.新疆雅丹地貌分布特征浅析[J].四川地质学报,2009,29(6):286-290.[15]吴正等.风沙地貌与治沙工程[M].北京:科学出版社,2003:111-115.[16]UNESCO.Operational guidelines for the implementation of the World Heritage convention[EB/OL].(2008-08-01)[2010-07-01].http://whc.unesco.org/en/guidelines.[17]姜红忠.雅丹地貌生态地质旅游价值探讨——以新疆哈密魔鬼城为例[J].新疆有色金属,2004,(增刊):9-10.[18]范广洲,程国栋.青藏高原隆升对西北干旱气候形成影响的模拟(Ⅰ):对大气环流影响[J].高原气象,2003,22(增刊):45-56.[19]范广洲,程国栋.青藏高原隆升对西北干旱气候形成影响的模拟(Ⅱ):水汽收支及高原动力、热力作用的影响[J].高原气象,2003,22:58-66.[20]薛积彬,钟巍,赵引娟,等.东疆北部全新世气候不稳定性的湖泊沉积记录[J].中国沙漠,2008,28(4):648-655.[21]夏训诚.中国罗布泊[M].北京:科学出版社,2007:66-68,204-206.[22]俄有浩,苏志珠,王继和,等.库姆塔格沙漠综合科学考察成果初报[J].中国沙漠,2006,26(5):693-697.[23]敖爱玲.“诺门罕战争遗址”旅游开发价值评析[J].呼伦贝尔学报,2009,17(2):9-11.[24]曹俊,杨更.新疆罗布泊旅游资源特征[J].四川地质学报,2006,29:235-241.[25]赵星,李江海,王运.世界山脉遗产对比研究及对我国自然遗产申报的建议[J].地质论评,2007,53:165-167. |