复理石沉积

  • 网络flysch
复理石沉积复理石沉积
  1. GPRS业务的推出使得这一难题迎刃而解。海尔微第带的推覆构造、复理石沉积、华力西地块;

    General Packet Radio Service ( GPRS ) puts the axe in the helve . nappe structure , flysch deposit , Hercynian massif in the Helve-tides ;

  2. 海尔微第带的推覆构造、复理石沉积、华力西地块;

    Nappe structure , flysch deposit , Hercynian massif in the Helve-tides ;

  3. 印支期出现早期前陆盆地海相复理石沉积,由于早印支运动使T2砂泥岩揉褶成山,晚期前陆盆地夭折。

    The marine flysch deposition of early foreland basin appeared in Indosinian ; owing to early Indosinian movement the sand mudstones ( T 2 ) were folded into mountains , which made the late foreland basin be withered away ;

  4. 礼岷前陆盆地经历了早期深海&半深海的复理石沉积阶段和晚期陆相磨拉石沉积阶段。

    The Lixian-Minxian foreland basin undertook abyssal-bathyal flysch deposition at its earlier evolution stage and continental molasse stage at its later evolution stage .

  5. 重建的地层层序和沉积地质特征显示巴颜喀拉盆地主体三叠系复理石沉积是周缘前陆盆地。

    The stratigraphic sequences and sedimentological characteristics indicate that the main body of Bayan Har Basin is composed of Triassic flysch sediments deposited in a foreland basin during Triassic .

  6. 复理石沉积中夹较多的玄武岩,这与现代洋底不同,而与岛弧蛇绿岩层序有相似之处,代表早期初始洋盆型洋壳的残块;

    The flysch , with some basalts , is difference from modern ocean , but similar to arc-ophiolite sequence , represents relics of ocean crust in early ocean basin .

  7. 复理石的沉积作用发育在裂陷盆地年青底板上的看法被广泛接受。

    The deposition of flysch onto the young floors of chiasmic basins is widely accepted as certain .

  8. 在巴颜喀拉山群中发现遗迹化石33属54种,为深海Nereites遗迹相的典型代表,反映出复理石相深水沉积特征;

    33 genera and 54 species of trace fossil have been discovered in the Bayan Har Shan Group , and they are typical representatives of the abyssal Nereites ichnofacies , reflecting the features of the flysch facies deep-water sedimentary environment .

  9. 赣西南早古生代复理石地层的沉积相、环境和旋回

    Sedimentary facies , environments and cycles of the Early Paleozoic flysch in Southwest Jiangxi