continental margin

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

The multi-geochemical data analysis shows that the occurring tectonic environment is an active continental margin.

The source rock could be formed in the condition of relatively stable continental margin epicontinental marine in micro-plate.

The tectonic setting is the combination of island arc related to a continent and an active continental margin.

The data and graphs from petrochemistry and geochemistry approve that the tectonic setting is continental margin arc.

Exploration maturity is relatively low in the continental margin of the northern South China Sea.

There is potential for petroleum exploration around the Manjaer original continental margin.

it constitutes a volcanic-sedimentary formation in the Late Paleozoic continental margin.

It caused the Youjiang Basin evolved from continental rift basin to passive continental margin rift basin.

Songliao basin is located in north west of the Pacific continental margin, its main area lies in the middle of Heilongjiang plates.

While the plotted points of the major compounds in Cretaceous sand-shale are mainly located in active continental margin area.

Therefore, the Kuruktag ur-ocean rift and Manjaer original continental margin were proposed.

It is located in the rift of continental margin.

Teng, Louis S. (1992) Geotectonic evolution of Tertiary continental margin basins of Taiwan. Petroleum Geology of Taiwan, 27, 1-19.

Statement of Understanding Concerning a Specific Method to be Used in Establishing the Outer Edge of the Continental Margin;

Petrology and geochemistry of an active continental margin intrusive rock belt on the northern margin of the Tarim plate

Metallogenetic System of Gold and Polymetallic Deposits along the Active Continental Margin on the Southern Edge of Qaidam Basin

Characteristics of Early Jurassic igneous rocks on the continental margin of southeastern China and their tectonic significance

Reservoir type and sedimentary evolution in the continental margin deepwater area of the northern South China Sea

The Late Precambrian Hot Water Sedimentation of the Southeast Yangtze Plate Continental Margin

Characteristics and evolution of active continental margin during early palaeozoic era in southern ordos

Tectonic framework and Meso-Cenozoic evolution of the East Asian continental margin

Metallogenic systems and belts developed on the late Paleozoic continental margin in Xinjiang

A Review of Gas Hydrate on the Passive Continental Margin and Its Pool-formation Process

Discussion on the Extension Model for the Conjugate Continental Margin of South China Sea

Opening of the South China Sea by Dextral Splitting of the East Asian Continental Margin

Translation company Outer edge of the continental margin;

Deepwater area-the new prospecting targets of northern continental margin of South China Sea

passive continental margin-cabonate rock platform stage since Sinian and Middle Triassic period;

Tectonics of subduction zone in the East Asia continental margin

The Study on Diatom of Late Quaternary Sediment in the Continental Margin of the East China Sea (Northern Fujian Member)

extensional continental margin type, such as the Southeast China extensional margin and the Basin and Range Province, USA;

Gas Hydrate in the Continental Margin Sediments

Slab Window in the Active Continental Margin