1) Middle Permian
中二叠世
1.
Geobiological Interpretation of the Oxygen-Deficient Deposits of the Middle Permian Marine Source Rocks in South China: A Working Hypothesis;
从地球生物学角度讨论华南中二叠世海相烃源岩缺氧沉积环境成因模式
2.
The discovery and significance of the Middle Permian adakites along the Huandong River north of the Xijir Ulan Lake,Qinghai;
青海西金乌兰还东河中二叠世埃达克岩的发现及其意义
3.
Middle Permian Fish Microremains from the Sidazhai Area,Ziyun County,Guizhou Province
贵州紫云四大寨地区中二叠世鱼类微体化石
2) middle and late Permian
中、晚二叠世
1.
The middle and late Permian faunas from the west Qinling Mountains have suffered a replacement event during the developing history.
西秦岭地区中、晚二叠世的生物,在其发展过程中经历了一次动物群的更替事件,表现为中二叠世茅口晚期迭山组底部开始的竺蜓类化石的突然锐减或消失及腕足动物的大量繁盛。
3) early-middle Permian
早-中二叠世
1.
The early-middle Permian epoch is a vital period during the sedimentary-tectonic evolution history,which is significant to the evolution history of South Tien orogenic belt, as well as the oil-gas geological conditions of northwestern margin of the Tarim basin in upper Paleozoic erathem.
塔里木盆地西北缘及其相邻的南天山造山带内蕴藏着丰富的矿产资源,保存有古亚洲洋与塔里木地块形成演化的重要信息,早-中二叠世是该地区沉积-构造演化史上发生重要变革的关键时期,对南天山造山带碰撞造山的演化历史和塔里木盆地西北缘地区上古生界的油气地质特征都具有重要意义。
5) Late Permian to Middle Triassic
晚二叠世-中三叠世
6) late middle Permian
中二叠世晚期
1.
Evolution of Brachiopod Diversity of the Late Middle Permian in the Hechuan Area of Chongqing;
重庆合川地区中二叠世晚期腕足动物多样性演变
2.
Based on the analysis on brachiopod fossils of the late middle Permian,the brachiopod extinction in Pre-Lopingian event of late middle Permian in this area can be divided into two sub screens: the first screen in the end of earlier Wushisanti Subage a.
通过川渝地区中二叠世晚期的腕足动物化石资料的研究,表明本地区中二叠世晚期的乐平世事件中腕足动物的灭绝可划分为前后2个不同的次级幕:早期的五十三梯亚期之末的第一幕和晚期的倒钻岩亚期之末的第二幕,且第二幕的灭绝规模要比第一幕更大。
补充资料：中中新世山旺盆地生态复原图
赵野木绘
[图]
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条