河北太行山中段地质特征及地学实践价值研究
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摘要
河北太行山中段,交通便利,山地、河流、丘陵等地貌类型多样,太古界、元古界、古生界、新生界等地层出露比较齐全,金属矿产、能源矿产、旅游风景等地质地貌资源丰富,断层、褶皱、节理等构造现象发育,是开展地质实践教学的有利场所。经过多年的教学研究和科学探索,河北地质大学目前分别在井陉县和临城县建立了两个地学实践教学基地,开辟了18条地质路线,编著了两部实践教材,开展的实践教学项目涉及地质认识、构造地质、地质填图、矿床地质、物化探、水文地质、旅游地质等多个方向。
There are convenient transportation and various geomorphological types such as mountains, rivers and hills, in middle Taihang Mountains, Hebei Province, China. The strata of Archaeozoic, Proterozoic, Paleozoic and Cenozoic, are relatively complete. At the same times, the geological and geomorphological resources such as metal minerals, energy minerals and tourist sceneries are abundant in this area. The structural outcrops such as faults,folds and joints are plenty too. Thus we can see that the research area is a favorable place for practical teaching of geology. After many years of teaching research and scientific study, two practical teaching bases in Jingxing County and Lincheng County has been established by Hebei GEO University. Two practical teaching materials and18 geological routes have been completed. Many practical teaching projects such as geological cognition practice,tectonic geology practice, geological mapping practice, ore deposit geology practice, physicochemistry exploration practice, hydrogeology practice, tourism geology practice, and so on, can be carried out in middle Taihang Mountains.
There are convenient transportation and various geomorphological types such as mountains, rivers and hills, in middle Taihang Mountains, Hebei Province, China. The strata of Archaeozoic, Proterozoic, Paleozoic and Cenozoic, are relatively complete. At the same times, the geological and geomorphological resources such as metal minerals, energy minerals and tourist sceneries are abundant in this area. The structural outcrops such as faults,folds and joints are plenty too. Thus we can see that the research area is a favorable place for practical teaching of geology. After many years of teaching research and scientific study, two practical teaching bases in Jingxing County and Lincheng County has been established by Hebei GEO University. Two practical teaching materials and18 geological routes have been completed. Many practical teaching projects such as geological cognition practice,tectonic geology practice, geological mapping practice, ore deposit geology practice, physicochemistry exploration practice, hydrogeology practice, tourism geology practice, and so on, can be carried out in middle Taihang Mountains.
引文
[1]王立峰.张河湾地质-旅游实习教程[M].北京:地质出版社,2010.
[2]王青春,胡胜军,史继忠,等.秦皇岛地质认识实习教程(第二版)[M].北京:地质出版社, 2016.
[3]李声之,许洪才.对河北省太古宙地层及主要构造事件的划分[J].北京地质, 1995(4):8-26.
[4]徐杰,高战武,宋长青,等.太行山山前断裂带的构造特征[J].地震地质, 2000, 22(2):111-122.
[5]朱光,胡召齐,陈印,等.华北克拉通东部早白垩世伸展盆地的发育过程及其对克拉通破坏的指示[J].地质通报, 2008,27(10):1594-1604.
[6]李俊建,罗镇宽,燕长海,等.华北陆块的构造格局及其演化[J].地质找矿论丛, 2010, 25(2):89-100.
[7]曹现志,李三忠,刘鑫,等.太行山东麓断裂带板内构造地貌反转与机制[J].地学前缘, 2013, 20(4):88-103.
[8]安慧婷,许立青,李三忠,等.太行山东麓断裂带中、新生代构造应力场及转换机制[J].大地构造与成矿学, 2015, 39(4):571-586.
[9]王立峰,于延秋,李冬,等.临城歧山湖矿产勘查实习教程[M].北京:地质出版社, 2018.
[10]牛树银,邵济安,孙爱群,等.华北东部盆山耦合与内生成矿作用[J].大地构造与成矿学, 2006, 30(3):331-342.
[11]李中念,张振芳,严国栋.河北省超贫磁铁矿资源与开发利用分析[J].河北冶金, 2006(3):1-4.
[12]毕伏科,肖文暹.河北省成矿区带和找矿远景区[J].地质调查与研究, 2006, 29(2):107-114.
[13]张道忠,刘志明,薛浩江,等.太行山南段甘陶河群铜矿化特征及控矿因素分析[J].矿产与地质,2007, 21(2):158-163.
[14]薛浩江,刘志明,朱梅花,等.太行山南段甘陶河群地层的地球化学异常特征及找矿意义[J].地质找论丛, 2009, 24(3):255-259.
[15]张亚东,宋金素,龚红雷,等.河北省铁矿分布与重磁场特征的关系[J].物探与化探, 2012, 36(4):517-522.
[16]吴忱.华北山地的水系变迁与新构造运动[J].华北地震科学,2001, 19(4):1-6.
[17]刘英学,景彦亭.临城水库水质变化趋势分析[J].地下水,2013, 35(6):123-125.
[18]白翠玲,鲁绍伟,杨建朝.水利旅游资源开发研究——以张河湾水库为例[J].安徽农业科学, 2008, 36(14):6013-6015.
[19]张晓曼,王健,郑倩华,等.河北临城崆山白云洞溶洞地貌和沉积特征及其影响因素[J].古地理学报, 2013, 15(1):49-58.
[20]郑倩华,王健,张晓曼,等.河北省崆山白云洞成因与演化[J].地球科学进展, 2013, 28(1):86-93.
[21]侯心羽,王一珉.浅析苍岩山桥楼殿的建筑构造和山林寺院的美学内涵[J].艺术与设计(理论),2017, 146:84-86.
[22]王青春,贺萍,杜江民,等.太行山中南段长城系赵家庄组地层沉积特征[J].西南石油大学学报(自然科学版), 2017, 39(4):47-56.
[23]童亨茂.野外地质教学中的科学管理与团队建设——野外地质教学二十年的经验和体会[J].中国地质教育, 2013(2):145-148.
[24]贺萍,王青春,刘汝敏,等.野外工作和旅游过程中的潜在危险——泥石流地质灾害[J].资源环境与工程, 2008, 22(3):339-341.
[25]王青春,贺萍.野外地质实践教学“安全、高效”运行方法[J].石家庄经济学院学报, 2014, 37(5):138-140.
[2]王青春,胡胜军,史继忠,等.秦皇岛地质认识实习教程(第二版)[M].北京:地质出版社, 2016.
[3]李声之,许洪才.对河北省太古宙地层及主要构造事件的划分[J].北京地质, 1995(4):8-26.
[4]徐杰,高战武,宋长青,等.太行山山前断裂带的构造特征[J].地震地质, 2000, 22(2):111-122.
[5]朱光,胡召齐,陈印,等.华北克拉通东部早白垩世伸展盆地的发育过程及其对克拉通破坏的指示[J].地质通报, 2008,27(10):1594-1604.
[6]李俊建,罗镇宽,燕长海,等.华北陆块的构造格局及其演化[J].地质找矿论丛, 2010, 25(2):89-100.
[7]曹现志,李三忠,刘鑫,等.太行山东麓断裂带板内构造地貌反转与机制[J].地学前缘, 2013, 20(4):88-103.
[8]安慧婷,许立青,李三忠,等.太行山东麓断裂带中、新生代构造应力场及转换机制[J].大地构造与成矿学, 2015, 39(4):571-586.
[9]王立峰,于延秋,李冬,等.临城歧山湖矿产勘查实习教程[M].北京:地质出版社, 2018.
[10]牛树银,邵济安,孙爱群,等.华北东部盆山耦合与内生成矿作用[J].大地构造与成矿学, 2006, 30(3):331-342.
[11]李中念,张振芳,严国栋.河北省超贫磁铁矿资源与开发利用分析[J].河北冶金, 2006(3):1-4.
[12]毕伏科,肖文暹.河北省成矿区带和找矿远景区[J].地质调查与研究, 2006, 29(2):107-114.
[13]张道忠,刘志明,薛浩江,等.太行山南段甘陶河群铜矿化特征及控矿因素分析[J].矿产与地质,2007, 21(2):158-163.
[14]薛浩江,刘志明,朱梅花,等.太行山南段甘陶河群地层的地球化学异常特征及找矿意义[J].地质找论丛, 2009, 24(3):255-259.
[15]张亚东,宋金素,龚红雷,等.河北省铁矿分布与重磁场特征的关系[J].物探与化探, 2012, 36(4):517-522.
[16]吴忱.华北山地的水系变迁与新构造运动[J].华北地震科学,2001, 19(4):1-6.
[17]刘英学,景彦亭.临城水库水质变化趋势分析[J].地下水,2013, 35(6):123-125.
[18]白翠玲,鲁绍伟,杨建朝.水利旅游资源开发研究——以张河湾水库为例[J].安徽农业科学, 2008, 36(14):6013-6015.
[19]张晓曼,王健,郑倩华,等.河北临城崆山白云洞溶洞地貌和沉积特征及其影响因素[J].古地理学报, 2013, 15(1):49-58.
[20]郑倩华,王健,张晓曼,等.河北省崆山白云洞成因与演化[J].地球科学进展, 2013, 28(1):86-93.
[21]侯心羽,王一珉.浅析苍岩山桥楼殿的建筑构造和山林寺院的美学内涵[J].艺术与设计(理论),2017, 146:84-86.
[22]王青春,贺萍,杜江民,等.太行山中南段长城系赵家庄组地层沉积特征[J].西南石油大学学报(自然科学版), 2017, 39(4):47-56.
[23]童亨茂.野外地质教学中的科学管理与团队建设——野外地质教学二十年的经验和体会[J].中国地质教育, 2013(2):145-148.
[24]贺萍,王青春,刘汝敏,等.野外工作和旅游过程中的潜在危险——泥石流地质灾害[J].资源环境与工程, 2008, 22(3):339-341.
[25]王青春,贺萍.野外地质实践教学“安全、高效”运行方法[J].石家庄经济学院学报, 2014, 37(5):138-140.