甜水海岔路口地区早石炭世地层化石的发现和帕斯群的建立  

Discovery of the Early Carboniferous fossils of brachiopods and corals and establishment of the Lower Carboniferous Pasi Group in the Chalukou region,Tianshuihai microcontinent,Xinjiang

作　　者：崔建堂 边小卫 王炬川 杨克俭 朱海平 王满仓 孔文年 

机构地区：[1]陕西省地质调查院,陕西咸阳712000

出　　处：《沉积与特提斯地质》2008年第1期55-58,共4页Sedimentary Geology and Tethyan Geology

基　　金：中国地质调查局1:25万康西瓦;岔路口等四幅区域地质调查项目(200313000003)

摘　　要：在1∶25万岔路口幅区域地质填图时,在原划中泥盆统落石沟组中采到了大量腕足、珊瑚类化石,经鉴定其成时代为早石炭世中期。该套地层可与西邻区域地层进行对比,对此新建下石炭统帕斯群。Abundant Early Carboniferous fossils of brachiopods and corals were collected from the formerly Middle Devonian Luoshigou Formation during the geological mapping of the 1 ： 250 000 Chalukou Sheet, Xinjiang. These fossils are dated at the middle Early Carboniferous, and the strata in which the fossils occur are redelineated as the Lower Carboniferous Pasi Group based on the stratigraphic correlation with the Shenxianwan Sheet west of it. This newly-established Pasi Group displays a fault contact with the underlying Lower Silurian Wenquangou Group and an angular unconformable contact with the overlying Lower Jurassic Bagongbulansayi Formation. The discovery of the Early Carboniferous fossils of brachiopods and corals and establishment of the Lower Carboniferous Pasi Group have filled up the space of the Early Carboniferous strata and provided new basic data for the refinement of the stratigraphic sequence framework and evolution on the Tianshuihai microcontinent.

关 键 词：甜水海块 岔路口 下石炭统 帕斯群 新疆 

分 类 号：P534.45[天文地球—古生物学与地层学]