安徽地质
安徽地質
안휘지질
GEOLOGY OF ANHUI
2013年
4期
253-255
,共3页
标志层%大巩山褶皱
標誌層%大鞏山褶皺
표지층%대공산습추
marker bed%the Dagong Mt fold
大巩山西堌堆组蚌埠期褶皱可利用含白云质大理岩透镜体的蛇纹岩作为标志层来恢复，推测其为轴面倒向北的紧密同斜褶皱，S0近南北向，枢纽西倾，地层由东向西变新。
大鞏山西堌堆組蚌埠期褶皺可利用含白雲質大理巖透鏡體的蛇紋巖作為標誌層來恢複，推測其為軸麵倒嚮北的緊密同斜褶皺，S0近南北嚮，樞紐西傾，地層由東嚮西變新。
대공산서고퇴조방부기습추가이용함백운질대리암투경체적사문암작위표지층래회복，추측기위축면도향북적긴밀동사습추，S0근남북향，추뉴서경，지층유동향서변신。
The Bengbu-period fold in Xigudui Formation in the Dagong Mt is recoverable using dolomitic marble lens-bearing serpentinite as marker bed. It was thought to be a tight isoclinal fold with its axial plane dipping north,S0 al-most NS,hinge plunging west and strata becoming younger to west from east.
