continental margin造句

Poor- or non-accretionary convergent continental margin

This paper deals with the features of late Middle Proterozoic active continental margin in South China.

The major disruption of Machaoying-Panhe defines the active continental margin of the north China plate and the south margin of the Epicontinental Sea in the Paleozoic period.

The South China Sea is one of the largest marginal seas in the western Pacific region, with its northern margin being characterized by a passive continental margin.

The major disruption of Heigou-Luanchuan has determined the active continental margin of the ancient north China plate.

Inversion structure features and their dynamic significances in Early Neogene strata at continental margin of the northeast South China Sea

This paper suggests that the north part of East Qinling is the continental marginal terrain on South Sinokorean plate, which is the active continental margin, characterized by double-lined island arc;

The existence of NW-SE direction mantle flow under the continental crust in the north continental margin of South China Sea made the extension activities migrate from north to south.

Located in middle part of the Jinshajiang tectonic belt, the Yangla copper orefield was in the clinoform area of an active continental margin.

Otherwise with Paleotethys closing in late Triassic period, the pull-apart continental margin reversed in Indo-China movement creating Indo-Chinafolded orogeny.

Like surrounding areas, the Jiangnan uplift belt in southern Anhui was situated on a passive continental margin during Sinian to Middle Triassic.

Tectono- sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.

and the Circum-Pacific metallogenic province into Upper Mesozoic ore-forming belt of the active continental margin and Paleocene-Pliocene ore-forming belt of the island arcs.

Xiaodushangxi tungsten deposit is located in the eastern end of the tarim plate, Beishan paleozoic continental margin activity with Liuyuan-Yu Well son with the western part of Rift Valley.

During the Neoproterozoic to the Early Paleozoic, the South China was a marginal basin captured by the Yangtze active continental margin, filled with very thick flysch, sandstone, and shale sediments.

There is not only mosaic structures consisting of small blocks and giant orogenic belts, but also modern continental margin with trenchs, island arc and basins lasting for 20 000 km.

Convergent (active) continental margins

Rifted (extensional, passive) continental margins

The coarse sediments have generally accumulated along the continental margins.

These are proper rear boundaries of continental margins, the geodynamics of which are characterized by rifting on shelves, continental slopes, and marginal oceanic depressions.

Geological characters of the East and West Africa continental margins and their significance for hydrocarbon exploration