South China Sea basin

Biology fountain is mainly plankton that constitutes the source rock of sea-facies in the South China Sea Basin , and kerogen type is III , which mainly generates gas .

南海盆地中生代生物源以浮游生物为主，干酪根为III型，以生气为主。

Distribution Characters and Exploration Potential of Mesozoic Sea Facies Sedimentary Strata in the South China Sea Basin

南海盆地中生代海相沉积地层分布特征及勘探潜力分析

A discussion on the origin and history of South China Sea Basin

南海海盆的形成演化探讨南海海盆新生代的构造演化史

Sediment Types and Sedimentation of the Central South China Sea Basin

南海中部沉积物类型和沉积作用特征

The Magnetostratigraphic Characteristics of some Shorter Cores from the Deep South China Sea Basin

南海深海短柱样的磁性地层学特征

Rate of accretion of manganese crust from the South China Sea Basin and its geochemical characteristics

我国南海海盆一块锰壳层的生长速度及某些地球化学特征

And ( 5 ) there is no space for the large-scale spreading of the South China Sea Basin .

南海海盆不具备大规模扩张的空间。

Geochemical differences between the oceanic crust of the South China Sea Basin and the ocean crust

南海中央海盆洋壳与大洋壳在地球化学上的差异性

The magnetic anomalies of the South China Sea Basin indicate that its oce .

南海盆地磁异常显示其洋壳是新老不一、厚薄不匀的新洋壳的拼合叠覆体。

Calculation on theoretical profiles of magnetic anomalies and preliminary analyses on magnetic lineation in South China Sea Basin

南海海盆磁异常理论剖面的计算和磁条带的初步分析

On the non island arc origins of the Taiwan island and its correlations with the South China sea basin

试论台湾岛的非岛弧成因及其与南海海盆的相关性

The faulting and the sedimentary history of the Baiyun Sag were also influenced by spreading in the South China Sea Basin .

白云凹陷的断裂活动和沉积演化史还受到南海海盆扩张活动的影响。

According to the opinion of " continental margin spreading " the paper presents a discussion on the original regime and evolutionary process of South China Sea Basin .

根据陆缘扩张理论，利用古地磁数据，结合地质、地球物理资料，对南海海盆的成因机制和演化过程进行探讨。

Generally bounding the Taiwan Straits , the East China Sea Basin belongs to the convergent margin evolved from a transform or passive margin and the South China Sea Basin belongs to the passive margin evolved from active or convergent margin .

大体以台湾海峡为界，东海盆地是一个由转换或被动边缘演化而来的聚敛边缘，而南海属于由活动或聚敛边缘转化而来的被动边缘。

Y. According to an analysis of tectonic evolution the Southern China continental margin basins belong to passive margin pull-apart basins and the South China Sea central basin belongs to margin sea basin .

根据构造演化分析，南缘的陆缘盆地属于不活动边缘拉裂盆地，南海中央海盆则属于边缘海盆地。

There have four kind of basins in the South China Sea area : rifting basin , strike-slip rifting basin , fore-land basin and fore-arc basin .

南海地区新生代沉积盆地有四类：张裂盆地、走滑拉张盆地、前陆盆地和前弧盆地。

Of them , the D_2 deformation shows a consistent forming time , extensional direction and tectonic regime amongst the Dulong-Song Chay dome , South China block and the north margin of the South China Sea basin .

D2期构造在发育时间、伸展方向及变形方式等上既与华南地块同时期区域伸展构造特征相一致，也与南海盆地北缘早期扩张特征相一致。

The spreading model of the South China Sea is questioned on the basis of integrated analyses and interpretation of geological and geophysical evidences in the South China Sea Basin and its vicinity from the view of plate tectonics , geology , geophysics and geodynamics .

从板块构造学、地球物理学和地球动力学等角度，结合南海中央海盆及其周边的地质、地球物理资料进行综合分析论证，对南海扩张成因模式提出质疑。