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1)  Proterozoic deformation
新元古代变形
2)  Neoproterozoic Era
新元古代
1.
The Discovery of Neoproterozoic Era Digging Trace Fossil in Huainan China and Its Geological Significance;
中国淮南新元古代掘迹化石发现及其意义
2.
The Study on Sedimentary Facies of Changlongshan Formation of Neoproterozoic Era in Huailai, Hebei;
河北省怀来新元古代长龙山组沉积相研究
3.
The epoch adscript to the Neoproterozoic Era and that the phosphorite bed located in the Sinian System.
海州—大悟地区变质磷矿含磷岩系(锦屏岩群、宿松岩群、红安岩群)岩层组合,标志岩层,微量、稀土元素特征和沉积环境皆可与鄂西陡山沱期磷矿类比,时代归属为新元古代,其中磷矿层属震旦系。
3)  Neoproterozoic
新元古代
1.
Geological characteristics,geochronology and tectonic settings of Neoproterozoic magmatic Ni-Cu-(PGE) sulfide deposits in China;
新元古代岩浆Ni-Cu-(PGE)硫化物矿床地质特征、形成时代及其地球动力学背景
2.
Extinct mechanism of the Neoproterozoic stromatolites from the Liulaobei Formation in the Huainan region, Anhui;
淮南地区新元古代刘老碑组叠层石消失原因初探
3.
Neoproterozoic slumping deposit in the Liulaobei Formation in the north of Anhui and its implication;
皖北新元古代刘老碑组滑塌沉积及其地质意义
4)  Xingxingxia rock group
新太古-古元古代
5)  Neoproterozoic metagranite
新元古代变质花岗岩
6)  Xiangshan Neo-Proterozoic metamorphic rocks
相山新元古代变质岩
1.
The Xiangshan Neo-Proterozoic metamorphic rocks are composed of argillo-arenaceous metamorphic rocks and amphibolites,of which the staurolite-garnet-mica,schist,quartz schist and leptynite have been studied geochemically,while the linear relations between some elements have also been investigated.
相山新元古代变质岩由泥砂质变质岩和斜长角闪岩组成。
补充资料:大坝内部变形观测(见水工建筑物变形观测)


大坝内部变形观测(见水工建筑物变形观测)


  daba neibubianxing guanCe大坝内部变形观测见水工建筑物变形观测。
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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