江苏十大地质遗迹评述
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摘要
通过对江苏省地质遗迹的详细调查,选出了江苏十大地质遗迹,即:宁镇山脉岩石地层建组层型剖面群,南京汤山古人类遗址及洞穴群,连云港—东海超高压变质带及科学深钻,南京六合火山群、雨花石群、石柱林群,溧阳上黄水母山高级灵长类及古哺乳动物化石遗址,泗州城地质灾害遗址,南京江宁娘娘山破火山口与碱性火山杂岩体,茅山薄皮构造—飞来峰,盐城海岸带变迁及湿地,太湖及周边地质遗迹。这些地质遗迹均具很高的科学价值、美学价值和稀有性,应加强保护,在保护中加以开发。
By a throughout investigation of geologic relics of Jiangsu Province, ten major geologic relics have been selected: a group of stratotype sections for lithostratigraphic formation in Ningzhen Mountain Chain; a cave cluster of paleoanthropological relics of Tangshan ,Nanjing; super high pressure metamorphic zone and super deep continental scientific drilling of Lianyungang-Donghai; volcano cluster,rock column forests and Yuhua gravels of Luhe, Nanjing; fossil relics of high-level primates and paleo-mammals at Shuimu Mountain, Shanghuang, Liyang county; geologic hazard relics in Sizhou county; Niangniangshan caldera and alkali volcanic complex in Jiangning county, Nanjing; thin-skinned structure-klippe of Maoshan Mountain; coast-line changing and marsh of Yancheng city; geologic heritage of Taihu Lake and its periphery. All of them are rare and of high scientific and aesthetic value, and should be put under intensive protection and be developed under protection.
By a throughout investigation of geologic relics of Jiangsu Province, ten major geologic relics have been selected: a group of stratotype sections for lithostratigraphic formation in Ningzhen Mountain Chain; a cave cluster of paleoanthropological relics of Tangshan ,Nanjing; super high pressure metamorphic zone and super deep continental scientific drilling of Lianyungang-Donghai; volcano cluster,rock column forests and Yuhua gravels of Luhe, Nanjing; fossil relics of high-level primates and paleo-mammals at Shuimu Mountain, Shanghuang, Liyang county; geologic hazard relics in Sizhou county; Niangniangshan caldera and alkali volcanic complex in Jiangning county, Nanjing; thin-skinned structure-klippe of Maoshan Mountain; coast-line changing and marsh of Yancheng city; geologic heritage of Taihu Lake and its periphery. All of them are rare and of high scientific and aesthetic value, and should be put under intensive protection and be developed under protection.
引文
[1] 江苏省地质矿产局.江苏省岩石地层单位[M].武汉:中国地质大学出版社,1997.
[2] 江苏省地方志编纂委员会.江苏省志·旅游业志[M].南京:江苏古籍出版社,1996.
[3] 吴汝康,李星学主编.南京直立人[M].南京:江苏科学技术出版社,2002.
[4] 汪永进,Haicheng,陆从伦,等.南京汤山洞穴碳酸盐沉积物的电离质谱铀系年代[J].科学通报,1999,44(14):15481551.
[5] ZhaoJX,HuK,CollersonKD,etal..ThermalionizationmassspectrometryU-seriesdatingofahominidsitenearNanjingChina[J].Geology,2001,29(1):27 30.
[6] XuZ,YangW,YangJ,etal..ChinesecontinentalscientificdrillingprogramintheSuluultrahighpressuremetamorphicbelt[J].ICDPNewsletter2000,2:13 16.
[7] 许志琴,张泽明,刘福来,等.苏鲁高压、超高压变质带的折返构造及折返机制[J].地质学报,2003,77(4):433 450.
[8] 徐红.南京六合桂子山玄武岩石桂林成因初探[J].地质论评,1999,45(增刊):703 706.
[9] 池澄,姚群.天赐国宝雨花石[M].南京:南京出版社,2000.
[10] K.ChristopherBeard,TaoQi,MaryR.Dawson,etal.AdiversenewprimatefaunafrommiddleEocenefissure-fillingsinSouthearthernChina[J].Nature,1994,368(14):604 609.
[11] 齐陶,K·克里斯托弗·毕尔德,王伴月,等.江苏溧阳上黄中始新世哺乳动物群的发现与意义[J].古背椎动物学报,1996,34(3):27 278.
[12] 赵剑畏.试论古泗州城遗址的地学内涵[A].中国旅游地学研究会陈安泽,卢云亭,陈兆棉主编.旅游地学的理论与实践—旅游地学论文集第七集[C].北京:中国林业出版社,2000,519 524.
[13] 陶奎元,黄光昭,王美星.南京娘娘山杂岩及其成因[J].中国地质科学院院报,1979,1:121 132.
[14] 陈贵志.论南京娘娘山碱性火山岩—侵入杂岩特征及成岩定量模拟[J].岩石矿物学杂志,1989,11(4):402 408.
[15] 孙竟雄,韦钧国.江苏西南部茅山推覆构造的基本特征[J].南京地质矿产研究所所刊,1985,6(3):27 41.
[16] 胡连英,徐学思,孙寿成,等.溧阳地震与茅东断裂带[M].北京:地震出版社,1997.
[17] 朱大奎,许廷官.江苏中部海岸发育和开发利用问题[J].南京大学学报(自然科版),1982,3:799 817.
[18] 陶奎元.盐城湿地与生态旅游[J].火山地质与矿产,2001,20(2):150 156.
[2] 江苏省地方志编纂委员会.江苏省志·旅游业志[M].南京:江苏古籍出版社,1996.
[3] 吴汝康,李星学主编.南京直立人[M].南京:江苏科学技术出版社,2002.
[4] 汪永进,Haicheng,陆从伦,等.南京汤山洞穴碳酸盐沉积物的电离质谱铀系年代[J].科学通报,1999,44(14):15481551.
[5] ZhaoJX,HuK,CollersonKD,etal..ThermalionizationmassspectrometryU-seriesdatingofahominidsitenearNanjingChina[J].Geology,2001,29(1):27 30.
[6] XuZ,YangW,YangJ,etal..ChinesecontinentalscientificdrillingprogramintheSuluultrahighpressuremetamorphicbelt[J].ICDPNewsletter2000,2:13 16.
[7] 许志琴,张泽明,刘福来,等.苏鲁高压、超高压变质带的折返构造及折返机制[J].地质学报,2003,77(4):433 450.
[8] 徐红.南京六合桂子山玄武岩石桂林成因初探[J].地质论评,1999,45(增刊):703 706.
[9] 池澄,姚群.天赐国宝雨花石[M].南京:南京出版社,2000.
[10] K.ChristopherBeard,TaoQi,MaryR.Dawson,etal.AdiversenewprimatefaunafrommiddleEocenefissure-fillingsinSouthearthernChina[J].Nature,1994,368(14):604 609.
[11] 齐陶,K·克里斯托弗·毕尔德,王伴月,等.江苏溧阳上黄中始新世哺乳动物群的发现与意义[J].古背椎动物学报,1996,34(3):27 278.
[12] 赵剑畏.试论古泗州城遗址的地学内涵[A].中国旅游地学研究会陈安泽,卢云亭,陈兆棉主编.旅游地学的理论与实践—旅游地学论文集第七集[C].北京:中国林业出版社,2000,519 524.
[13] 陶奎元,黄光昭,王美星.南京娘娘山杂岩及其成因[J].中国地质科学院院报,1979,1:121 132.
[14] 陈贵志.论南京娘娘山碱性火山岩—侵入杂岩特征及成岩定量模拟[J].岩石矿物学杂志,1989,11(4):402 408.
[15] 孙竟雄,韦钧国.江苏西南部茅山推覆构造的基本特征[J].南京地质矿产研究所所刊,1985,6(3):27 41.
[16] 胡连英,徐学思,孙寿成,等.溧阳地震与茅东断裂带[M].北京:地震出版社,1997.
[17] 朱大奎,许廷官.江苏中部海岸发育和开发利用问题[J].南京大学学报(自然科版),1982,3:799 817.
[18] 陶奎元.盐城湿地与生态旅游[J].火山地质与矿产,2001,20(2):150 156.
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