Geology Of East Timor
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Geology Of East Timor
The geology of East Timor has been studied onshore and with offshore seismic studies. The region experienced rifting between the Permian and early Cretaceous. Shallow water sediments shifted to deep water sediments by the Triassic. The region was a subsiding passive margin from the Early Cretaceous through the Eocene, experiencing deep water carbonate and shale deposition. During the mid-Eocene, the Australian Plate collided with a subduction zone, generating folds and thrusts plus emplacing sheets of ophiolite and continental rock on top of Mesozoic sedimentary rocks. Some eroded sediments were shifted into a neighboring foredeep and these tectonic conditions produced oil-forming conditions in Triassic shales. Slow subsidence and carbonate deposition were typical of the region from the Eocene through the Miocene, until a second phase of thrusting uplifted onshore structures up to one kilometer. Offshore thrust sheets were buried beneath Pliocene and Pleistocene sediments. Referen ...
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East Timor
East Timor (), also known as Timor-Leste (), officially the Democratic Republic of Timor-Leste, is an island country in Southeast Asia. It comprises the eastern half of the island of Timor, the exclave of Oecusse on the island's north-western half, and the minor islands of Atauro and Jaco. Australia is the country's southern neighbour, separated by the Timor Sea. The country's size is . Dili is its capital and largest city. East Timor came under Portuguese influence in the sixteenth century, remaining a Portuguese colony until 1975. Internal conflict preceded a unilateral declaration of independence and an Indonesian invasion and annexation. Resistance continued throughout Indonesian rule, and in 1999 a United Nations–sponsored act of self-determination led to Indonesia relinquishing control of the territory. On 20 May 2002, as ''Timor-Leste'', it became the first new sovereign state of the 21st century. The national government runs on a semi-presidential system, w ...
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