English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

As a consequence of exploration for hydrocarbons, and of research programmes conducted by academic and international institutions, substantial progress has been made in recent years in definition of hydrocarbon-bearing basins, and those potentially so, in southeast Asia and especially in the vicinity of the South China Sea. Basins and depositional provinces now recognized include: the Thai Basin, the Khorat and Panjang Basins, the Malay Basin, West Natuna and Penyu Basins, Saigon (Ho Chi Minh) and Mekong (Vung Tau) Basins, East Natuna area, the Greater Sarawak Basin including Central Luconia and Balingian depositional provinces, the Baram Delta/Brunei-Sabah Basin and the Northwest Palawan Shelf. Where hydrocarbons have been encountered, the deposits are commonly associated with rocks of Middle and Upper Miocene age. Oliogene and Pliocene occurrences are locally significant. With some exceptions, most sedimentary basin-fill was deposited within continental to coastal environments. Such sediments are commonly gas-prone. Where oil-prone, there are suggestions that the oil has been generated under conditions of greater thermal maturity.

Review of principal hydrocarbon-bearing basins around the South China Sea