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利用XRD、XRF、FT-IR和Rs分析浙江缙云恐龙化石及围岩
引用本文:刘东亮,邓建国,彭光照,金幸生.利用XRD、XRF、FT-IR和Rs分析浙江缙云恐龙化石及围岩[J].信阳师范学院学报(自然科学版),2014(3):332-336.
作者姓名:刘东亮  邓建国  彭光照  金幸生
作者单位:1. 四川理工学院材料腐蚀与防护四川省重点实验室,四川自贡,643000
2. 自贡恐龙博物馆,四川自贡,643013
3. 浙江自然博物馆,浙江杭州,310014
基金项目:腐蚀与防护四川省重点实验室项目(2011CL12);四川理工学院培养项目
摘    要:通过XRF、XRD、FT-IR和RS对产自浙江缙云恐龙骨骼化石和围岩的元素组成、矿物结构和基团特征进行了分析.结果表明:化石中主要元素为钙、磷,钙磷质量比为12.7,围岩中硅、铁、钙、钾和铝含量较高;化石中钙含量是围岩的15倍,磷量为31.9倍,围岩中铁量是化石的8.5倍,硅含量是化石的11.25倍,钾含量是化石的45.6倍,铝含量是化石的7.36倍;恐龙化石的主要成分为羟基碳氟磷酸钙与碳酸钙,分别占63.9%和36.1%,围岩主要成分二氧化硅约为36.9%,其余为碳酸钙和硅酸盐的混合物.红外与拉曼峰表明,化石中存在羟基碳氟磷酸钙、方解石及少量有机物;有机物的存在表明,化石未被完全石化,且恐龙死亡后初始阶段埋藏在缺氧环境中;而围岩中则为石英、方解石和有机物.

关 键 词:恐龙骨骼化石  围岩  光谱分析  矿物成分

Analysis of Dinosaur Fossils and Surrounding Rocks from Jinyun Region by XRD,XRF, FT-IR and Rs
Liu Dongliang,Deng Jianguo,Peng Guangzhao,Jin Xingsheng.Analysis of Dinosaur Fossils and Surrounding Rocks from Jinyun Region by XRD,XRF, FT-IR and Rs[J].Journal of Xinyang Teachers College(Natural Science Edition),2014(3):332-336.
Authors:Liu Dongliang  Deng Jianguo  Peng Guangzhao  Jin Xingsheng
Institution:Liu Dongliang;Deng Jianguo;Peng Guangzhao;Jin Xingsheng;Material Corrosion and Protection Key Laboratory of Sichuan Province,Sichuan University of Sciences & Engineering;Zigong Dinosaur Museum;Zhejiang natural history Museum;
Abstract:X-ray fluorescence( XRF),X-ray diffraction( XRD),Fourier transform infrared( FTIR) and Raman spectroscopy were adopted to characterize the elements,mineral structures and groups of dinosaur fossils and surrounding rocks from Jinyun Zhejiang in China. The results showed that the main elements of the fossils are calcium and phosphorus. The ratio of calcium and phosphorus in fossils is 12. 7. The main elements in surrounding rocks are silicon,iron,calcium,potassium and aluminum. The components of calcium,phosphorus in fossils are 15 and 31. 9 times that in surrounding rocks,respectively. On the other hand,the components of iron,silicon,potassium and aluminum in surrounding rocks are 8. 5,11. 25,45. 6 and 7. 36 times that in fossils,respectively. The main contents of fossils are63. 9% hydroxyl carbonate-fluorapatite and 36. 1% calcium carbonate,while the contents of silica in surrounding rocks are 36. 9%,others are a mixture of calcium carbonate and silicate. The results from FTIR and Raman spectroscopy showed that there exist hydroxyl carbonate-fluorapatite,calcite and some organic matter. The organic matter indicated that the fossils do not fossilize completely. The analyses from mineral contents showed that there was lack of oxygen when the dinosaurs were buried. The results from FTIR and Raman spectroscopy also showed that the main contents are silica,calcium carbonate and organic matter.
Keywords:dinosaur fossils  country rocks  spectroscopic analysis  mineral composition
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