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1.Biostratigraphic division of the Upper Carboniferous to Middle Permian in Zhejiang
浙江省上石炭统—中二叠统生物地层划分进展收藏指正
2.Study on Early-Middle Permian Reef and Its Sequence Stratigraphy in Maerzheng Area, Eastern Kunlun
东昆仑马尔争早中二叠世生物礁及其层序地层研究收藏指正
3.The beginning of Misellina-Brevaxina acme zone is considered as the lower limit of Middle Permian.
Misellina-Brevaxina顶峰带的出现是中二叠统的底界,Codonofusiella 顶峰带的出现是上二叠统的底界。收藏指正
4.Study on the Origin of the Dolostone Intercalcated in the Black Shales in Middle Permian Lucaogou Formation Eastern Part of Southern Margin of Junggar Basin
准噶尔盆地南缘东部中二叠流芦草沟组黑色页岩中白云岩夹层的成因探讨收藏指正
5.As one of the typical cool water brachiopod, Anidanthus had a main time range between Sakmarian of the early Permian and Wordian of the middle Permian. Several pioneers appeared in Bashkirian of the late Carboniferous.
Anidanthus是凉水型腕足动物的代表之一 ,主要出现在早二叠世Sakmarian期至中二叠世Wordian期 ,先驱分子在晚石炭世的巴什基尔期已出现 ,部分种延至晚二叠世。收藏指正
6.The early Middle Permian (Qixian Stage) reefs are discovered only in the Glass Mountains of North America, Pamirs and Aerge Mountains in West China.
中二叠世栖霞期的礁仅发现于北美格拉斯山脉、帕米尔和我国的阿尔格山等地。收藏指正
7.One to three karst cycles may be recognized mostly at the top of the Upper Permian strata, top of the Middle Permian Maokouan strata and top of the Carboniferous strata and subordinately at the top of the Devonian strata.
这些古岩溶作用主要存在于上二叠统顶部、中二叠统茅口组顶部和石炭系顶部，其次是泥盆系的顶部。收藏指正
8.Based on comprehensive analysis of the outcrops and interpretation of seismic data in this area,six detachments are identified,which are the Middle Permian Lucaogou and Hongyanchi Formations,the Lower Jurassic Badaowan Formation,the Middle Jurassic Xishanyao Formation,the Cretaceous Tugulu Group,the Palaeocene Anjihaihe Formation and the Neocene Taxihe Formation from the deep to the shallow.
通过大量地表露头的观察和地震资料的解释,系统识别和厘定了中二叠统芦草沟组和红雁池组、下侏罗统八道湾组、中侏罗统西山窑组、白垩系吐谷鲁群、古近系安集海河组和新近系塔西河组等共6个与大套泥岩、膏泥岩和煤系地层相关的主要构造滑脱层。收藏指正
9.Take for example the Huangjiankeng-Hashu rich copper belt occurring on the contact surface between the base of the Emeishan basalt and limestone of the Middle Permian Maokou Formation, the paper discusses the geological conditions of this new type of basalt copper deposit and the effects of the eruption of the Emeishan basaltic magma on the concentration of elemental Cu (Au, Pb, Zn, Pt, Pd, Sb, Fe etc.) and modification of mineralization by late-stage hydrothermal fluids.
以峨眉山玄武岩底部与中二叠统茅口组灰岩接触界面上赋存的黄见坑-哈树富铜矿带为例,论述了这一新类型玄武岩铜矿的成矿地质条件及峨眉山玄武岩浆喷-溢对Cu(Au、Pb、Zn、Pt、Pd、Sb、F等)元素的富集和后期热液改造成矿作用,以扩大找矿思路。收藏指正
10.Mineral, palaeontology, middle devonian, permian to early jurassic, and cretaceous.
收藏矿物、古生物学、中泥盆纪、二叠纪到早期的侏罗纪和白恶纪。收藏指正
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