节点文献
广西布兵盆地第四纪地貌与地质发育历史
QUATERANRY GEOMORPHOLOGY AND GEOLOGICAL DEVELOPMENT OF THE BUBING BASIN IN GUANGXI,SOUTH CHINA
【作者】 田丰; 黄芬; 黄秋艳; 黄胜敏; 黄鑫; 谢绍文; 袁宝印; 黄慰文; 王頠;
【Author】 TIAN Feng~1 HUANG Fen~2 HUANG Qiuyan~1 HUANG Shengmin~2 HUANG Xin~3 XIE Shaowen~4 YUAN Baoyin~5 HUANG Weiwen~6 WANG Wei~4 1 Tiandong Museum of Guangxi,Tiandong 531500,Guangxi; 2 Ethnic Museum of Bose,Bose 533000,Guangxi; 3 Cultural Relics Management Department of Youjiang District,Bose 533000,Guangxi; 4 Natural History Museum of Guangxi,Nanning 530012,Guangxi; 5 Institute of Geology and Geophysics,Chinese Academy of Science,Beijing 100029; 6 Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of Science,Beijing 100044
【机构】 田东县博物馆; 右江民族博物馆; 百色市文物管理所; 广西自然博物馆; 中国科学院地质与地球物理研究所; 中国科学院古脊椎动物与古人类研究所;
【摘要】 位于广西田东和田阳县境内的布兵盆地,是百色盆地东南部边缘的一个小型附属盆地。盆地内部及其南部边缘发育11层喀斯特洞穴,洞穴堆积物中保存大量的哺乳动物化石、人类化石以及石制品,其时代包括2 Ma以来的多个时期。盆地内还发育4级河流阶地,第Ⅳ级阶地堆积物中含有旧石器及玻璃陨石。布兵盆地的发育始于白垩纪末、古近纪初喜马拉雅运动阶段,至少自第四纪以来,盆地处于间歇性抬升时期,形成多层洞穴和阶地。这些洞穴和河流堆积物对于研究华南第四纪环境变迁和生物演化等具有重要意义。
【Abstract】 Bubing basin,located at Tiandong and Tianyang County,is an adjunctive small basin at southeastern Bose basin.Karst caves are broadly developed at the limestone towers inside the basin,and southern marginal limestone Mils.So far,our five years research works in this basin have indicated that about 11 layers caves are at different elevations,varying in sediments and mammalian faunas deposited during several periods from early Pleistocene to Holocene,generally between 2 Ma to 500 a.Some of these caves are rich of Hominoid elements of Hylobates,Gigantopithecus,Pongo,Homo fossils and bone,tektites and stone artifacts.Four fluvial terraces are also distributed at the Bubing basin,the highest one contains stone artifacts and tektites in laterite sediment,which corresponds to the Bose basin stone industry morphologically and stratigraphically. Geological studies reveal the Bubing basin was primitively developed during the end of the Cretaceous period and the earlier Paleogene,and intermittently uplifted since beginning Quaternary at least.Numerous layers of caves and terraces were formed and situated at varying elevations.So,the cave deposits and terrace sediments are significant in study of Quaternary environmental changes and mammalian evolution in south China.
【Key words】 Karst caves; fluvial terraces; Quaternary geomorphology; geological development; Bubing basin;
- 【会议录名称】 第十一届中国古脊椎动物学学术年会论文集
- 【会议名称】第十一届中国古脊椎动物学学术年会
- 【会议时间】2008-09
- 【会议地点】中国山西太原
- 【分类号】Q911
- 【主办单位】中国古脊椎动物学会