1.One of the key subjects reported at the symposium is the Early Triassic chronostratigraphy, esp. the GSSP for the Induan-Olenekian boundary; the second is the expression and process of biotic and environmental events during the Permian-Triassic transition; the third is the calcimicrobialite and the specific ecosystems at the Permian-Triassic boundary and in the Early Triassic the fourth is the evolution and lineages of some key taxonomic groups in the Early Triassic; the fifth is the recovery process and pattern of the ecosystems at the beginning of the Mesozoic; and the sixth is the causes of the delayed biotic recovery in the Early Triassic.
学术主题之一是早三叠世年代地层格架，尤其是印度阶－奥伦尼克阶界线层型；第二是二叠纪－三叠纪之交灭绝和环境事件的表现形式和过程；第三是二叠纪－三叠纪之交及早三叠世微生物岩及其代表的特殊生态系；第四是灭绝事件后三叠纪初一些关键生物类别的演变历程；第五是中生代初生态系复苏过程和型式；第六是早三叠世生物迟滞复苏的原因。
2.The hydrocarbon source rocks of Anyuan Formation, Upper Triassic,have been exposed by well Pocan-1 drilled lately in Nanchang Seg, thus negating the traditional idea of lacking of Upper Triassic and indicating the existence of the new exploration domain of Upper Triassic in the seg.
首次在南昌凹陷钻探的鄱参1井揭露了上三叠统安源组烃源岩,否定了该区没有晚三叠世沉积的传统认识,预示了南昌凹陷存在上三叠统的勘探新领域。
3.Through the analysis of subsidence history in the north of western Ordos basin, as a result of the terranes northward accretion and the successive collision of the Baykala block in the Middle Triassic, the Qiangtang block in the Late Triassic, the Lhasa block in the Middle Jurassic, the Gangdese block in the Cretaceous and the subduction of Izanagi plate in Yanshanian period, the studied region became a intracontinental foreland basin from Late Triassic to Cretaceous.
摘要通过对鄂尔多斯盆地西缘北段沉降史的分析可知，晚三叠世－白垩纪，由于中三叠世巴颜喀拉地体、晚三叠世羌塘地体、中－晚侏罗世拉萨地块、白垩纪冈底斯地体连续向北增生、碰撞以及燕山期伊佐奈岐板块的俯冲，盆地西缘北段的响应显示为陆内前陆盆地的特征。
4.(6)The tectonic evolution of the Xidamingshan uplift can be mainly divided into three stages: Sinian period to Silurian period is the foundation evolution stage, Devonian period to mid-Triassic period is the regional extension-depression stage and late Triassic period to Cenozoic era is the compressional structural deformation and uplift-erosion stage.
(6)西大明山隆起的构造演化主要分为三个阶段:震旦纪-志留纪的基底构造演化阶段; 泥盆纪-中三叠世区域伸展裂陷阶段和晚三叠世-新生代挤压构造变形与隆升剥蚀阶段;
5.Based on the investigations of 46 species of fossil spores and pollen belonging to 28 genera which were found from the Yongping Formation and Wayaopu Formation of Upper Triassic in Tongchuan region of Shaanxi Province, the early to late Late Triassic palynoflora in the region was established.
摘要本文基于陕西铜川地区上三叠统水坪组和瓦窑堡组发现的孢子花粉化石28属46种的研究，建立了研究区晚三叠世早期至晚期孢粉植物群。
6. According to vertical distribution of Bivalve at Upper Triassic sections inLongchang of Zhenfeng and in Qingchang of Bine, Late Triassic Bivalve of Yangtzeprovince, Guizhou is divided into 8 biostratigraphic units, i.e., in ascending order,1. Halobia Kui- "Daonella" bifurata Ass.
根据贞丰龙场、毕节青场等上三叠统剖面上双壳类的垂直分布，结合区域资料，将贵州扬子地层区晚三叠世双壳类划分为8个生物地层单位。 自下而上为：①Halobikui-"Daonella"bifurcata组合带；
7.Due to its richness in hydrocarbon in the Late Triassic,the deformation age,characteristics and mechanism of the Late Triassic foreland basin were analyzed in detail,and the relationship between structural deformation and hydrocarbon accumulation was especially high lighted.
鉴于这一地区已经证实晚三叠世地层中富含油气 ,该文以获得的实际资料对晚三叠世前陆盆地形变年代、形变特征、形变运动 (动力 )学机制进行了深入分析 ,并着重分析了构造形变与油气成藏的关系。
8.Guanling fossil lagerst?tte found from the Late Triassic (Carnian) Xiaowa Formation of the Guanling area, Guizhou province, Southwest China has numerous well preserved Late Triassic (Carnian) crinoids and marine reptiles.
在中国贵州关岭地区晚三叠世(卡尼期)小凹组(=瓦窑组)海生爬行动物和海百合化石库中产有大量完好保存的创口海百合(Traumatocrinus)(棘皮动物门,海百合纲)化石。
9.In the area of the left bank, rock body is mainly composed of Permian Period-Triassic Period granite and Triassic Period siltstones and mudstones (T2m). Moreover, the rock body has been more faulted, such as F1 F3 F9 and so on. In addition, there also exist a lot of joints and form complex rock mass structure.
工程区主要出露二迭纪～三迭纪花岗岩体(γ_4~3～γ_5~1)和三迭系中统忙怀组下段沉积岩(T_(2m)~1)，发育有工程区规模最大的F_1和F_3断层，以及其它断层和大量的各类断续延伸的裂隙，岩体结构较为复杂。
10.EARLIEST TRIASSIC AMMONOID FAUNAS FROM JIANGSU AND ZHEJIANG AND THEIR BEARING ON THE DEFINITION OF PERMO-TRIASSIC BOUNDARY
论苏、浙一带三叠纪最早期的菊石群及二叠系—三叠系界线的定义
