1.
The research results show below: (1) The bark of Acacia spp.
结果表明:(1)相思树皮结构为叠生构造。
2.
concertina movement
折叠[蛇腹]式构造
3.
Sedimentary Tectonic Evolution from Late Palaeozoic to Triassic in the South of North China Block
华北地块南部晚古生代至三叠纪沉积构造演化
4.
nonsynchronous superposed arcuate structure
非同期叠加弧形构造
5.
Mesozoic-Cenozoic Superimposed Orogeny and Foreland Deformation in the Northeastern Sichuan Basin
四川盆地东北部中—新生代造山与前陆变形构造叠合关系研究
6.
It is the arc tectonic that had ever caused the Diexi earthquake with magnitude 7.5 in 1933 at the place where is on the western wing and near the top of the arc.
该弧形构造西翼靠弧顶部位 1933年曾发生过叠溪 7 5级地震。
7.
Basin Translation from Late Palaeozoic to Triassic of Youjiang Basin and Its Tectonic Significance
右江盆地晚古生代—三叠纪盆地转换及其构造意义
8.
The Late Paleozoic-Early Triassic sedimentary characteristics and its tectonic significance in southwestern Fujian,China
闽西南晚古生代─早三叠世沉积特征及其大地构造意义
9.
PERMIAN AND TRIASSIC TURBIDITE AND ITS TECTONIC SIGNIFICANCE IN THE NORTHWESTERN ZHEJIANG
浙西北二叠、三叠纪浊积岩系及其大地构造意义
10.
Key Tectonic Changes and Staging Differential Structural Deformation in Superimposed Basins
叠合盆地关键构造变革期与分期差异构造变形
11.
Tectonic Evolution and Its Control for Hydrocarbon Accumulation of Mesozoic-Cenozoic Multicycle Superimposed Reformation Basin in the West of Northern Qaidam Basin;
柴达木北缘西段中、新生代多旋回叠加改造型盆地构造演化及对油气成藏的控制作用
12.
IMBRICATED AMALGAMATION TECTONICS IN EARLY PRECAMBRIAN CRATONS
早前寒武纪克拉通内的叠瓦拼贴构造
13.
Tectonic-sequence-based Lithofacies and Paleogeography of Permian in South of China
中国南方二叠纪构造—层序岩相古地理
14.
Permo-Carboniferous Coalfield Coal-Control Structure Features in Hebei Province
河北省石炭—二叠纪煤田控煤构造特征
15.
The Closure Time of the Paleo-Asian Ocean and the Paleo-Tethys Ocean:Implication for the Tectonic Cause of the End-Permian Mass Extinction
古亚洲洋和古特提斯洋的闭合时代——论二叠纪末生物灭绝事件的构造起因
16.
Re-discussion of the Seismogenic Structure of the Diexi Large Earthquake in 1933 and the Arc Tectonics on Jiaochang,Sichuan Province
四川较场弧形构造与1933年叠溪地震发震构造的再讨论
17.
Geochemistry Discrimination of Late Triassic Volcanic Rocks in Changdu-Simao Tectonic Zone
昌都-思茅构造带晚三叠世构造环境的火山岩地球化学判别
18.
This sediment will then probably be formed into a folded and imbricated structure.
然后这些沉积物可能形成褶皱和叠瓦构造。