Question: Katine is located ina country that lies in what basin?

Context articles: Niger Delta Basin (geology)
Persian Gulf Basin
Los Angeles Basin
Uganda
Bransfield Basin
Woodlark Basin
Turlock Basin
Katine
Rajasthan Basin
Geology of southern North Sea

The Niger Delta Basin, also referred to as the Niger Delta province, is an extensional rift basin located in the Niger Delta and the Gulf of Guinea on the passive continental margin near the western coast of Nigeria with suspected or proven access to Cameroon, Equatorial Guinea and São Tomé and Príncipe.
 This basin is very complex, and it carries high economic value as it contains a very productive petroleum system.
 The Niger delta basin is one of the largest subaerial basins in Africa.
 It has a subaerial area of about 75,000 km, a total area of 300,000 km, and a sediment fill of 500,000 km.
 The sediment fill has a depth between 9–12 km.
 It is composed of several different geologic formations that indicate how this basin could have formed, as well as the regional and large scale tectonics of the area.
 The Niger Delta Basin is an extensional basin surrounded by many other basins in the area that all formed from similar processes.
 The Niger Delta Basin lies in the south westernmost part of a larger tectonic structure, the Benue Trough.
 The other side of the basin is bounded by the Cameroon Volcanic Line and the transform passive continental margin.
The Persian Gulf Basin, is found between the Eurasian and the Arabian Plates.
 The Persian Gulf is described as a shallow marginal sea of the Indian Ocean that is located between the south western side of Iran and the Arabian Peninsula and south and southeastern side of Oman and the United Arab Emirates.
 Other countries that border the Persian Gulf basin include; Saudi Arabia, Qatar, Kuwait, Bahrain and Iraq.
 The Gulf extends a distance of 1000 km with an area of 240,000 square km.
 The Persian Gulf basin is a wedge-shaped foreland basin which lies beneath the western Zagros thrust and was created as a result of the collision between the Arabian and Eurasian plates.
The Los Angeles Basin is a sedimentary basin located in southern California, in a region known as the Peninsular Ranges.
 The basin is also connected to an anomalous group of east-west trending chain of mountains collectively known as the California Transverse Ranges.
 The present basin is a coastal lowland area, whose floor is marked by elongate low ridges and groups of hills that is located on the edge of the Pacific plate.
 The Los Angeles Basin, along with the Santa Barbara Channel, the Ventura Basin, the San Fernando Valley, and the San Gabriel Basin, lies within the greater southern California region.
 On the north, northeast, and east, the lowland basin is bound by the Santa Monica Mountains and Puente, Elysian, Repetto hills.
 To the southeast, the basin is bordered by the Santa Ana mountains and the San Joaquin Hills.
 The western boundary of the basin is marked by the Continental Borderland and is part of the onshore portion.
 The California borderland is characterized by north-west trending offshore ridges and basins.
 The Los Angeles Basin is notable for its great structural relief and complexity in relation to its geologic youth and small size for its prolific oil production.
 Yerkes et al. identify 5 major stages of the basin's evolution that begins in the Upper Cretaceous and ends in the Pleistocene.
 This basin can be classified as an irregular pull-apart basin accompanied by rotational tectonics during the post-early Miocene.
Uganda ( or ), officially the Republic of Uganda, is a landlocked country in East Africa.
 It is bordered to the east by Kenya, to the north by South Sudan, to the west by the Democratic Republic of the Congo, to the south-west by Rwanda, and to the south by Tanzania.
 The southern part of the country includes a substantial portion of Lake Victoria, shared with Kenya and Tanzania.
 Uganda is in the African Great Lakes region.
 Uganda also lies within the Nile basin, and has a varied but generally a modified equatorial climate.
The Bransfield Basin is a back-arc rift basin located off the Northern tip of the Antarctic Peninsula.
 The basin lies within a Northeast and Southwest trending strait that separates the peninsula from the nearby South Shetland Islands to the Northwest.
 The basin extends for more than 500 km from Smith Island (South Shetland Islands) to a portion of the Hero Fracture Zone.
 The basin can be subdivided into three basins: Western, Central, and Eastern.
 The Western basin is 130 km long by 70 km wide with a depth of 1.3 km , the Central basin is 230 km long by 60 km wide with a depth of 1.9 km , and the Eastern basin is 150 km long by 40 km wide with a depth of over 2.7 km .
 The three basins are separated by the Deception Island and Bridgeman Island.
 The moho depth in the region has been seismically interpreted to be roughly 34 km deep.
The Woodlark Basin is a geologic structural basin located in the southwestern Pacific Ocean and can be found to the southwest of the island country of Papua New Guinea.
 The basin is an extensional basin that is actively spreading and has a seafloor spreading center.
 This basin lies between the Indo-Australian Plate and the Solomon microplate and is located at 09°S, 155°E.
 The Woodlark Basin has an interesting geologic history dating back twenty million years to the initial opening of the basin; the spreading of the basin, however, has occurred within the past three million years.
 Due to the relatively young age of the basin, many researchers are interested in learning how the basin will continue to develop over time and how the plates will subduct.
 The subduction of the plates in the Woodlark Basin will be unique because the new crust being formed will be young and warm unlike most crust that gets subducted due to its low temperature and high density.
The Turlock Basin is a sub-basin of the San Joaquin Valley groundwater basin which occupies approximately 13,700 total square miles, making it the largest groundwater basin in California.
 The Turlock Basin makes up 542 square miles (347,000 acres) of this total.
 This aquifer is located within Merced and Stanislaus counties in the Central Valley bounded by the Tuolumne River to the north, the Merced River to the south and San Joaquin River to the west.
 The Sierra Nevada foothills bound the sub-basin to the east.
 Groundwater in the San Joaquin Valley occurs mostly in younger alluvial material.
 The Turlock Basin lies to the east of the city of Turlock.
 Groundwater in the Turlock Basin occurs in older alluvial deposits.
 Large portions of the San Joaquin Basin have experienced overdraft of water and infiltration of agricultural water pollutants, resulting in poor water quality.
Katine is a sub-county in the Soroti District of Uganda.
 It contains 66 villages, one of which is also called Katine.
The Rajasthan Basin is a sedimentary basin located in the north west part of India.
 This sedimentary basin is one of India’s major sources of petroleum and natural gas and has a geographical extent of about 126,000 sqkm .
 The Rajasthan Basin unconfirmably lies over a pre-Cambrian basement.
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The North Sea basin is located in NE Europe and lies between the United Kingdom, and Norway just north of The Netherlands and can be divided into many sub-basins.
 The Southern North Sea basin is the largest gas producing basin in the UK continental shelf, with production coming from the lower Permian sandstones which are sealed by the upper Zechstein salt.
 The evolution of the North Sea basin occurred through multiple stages throughout the geologic timeline.
 First the creation of the Sub-Cambrian peneplain, followed by the Caledonian Orogeny in the late Silurian and early Devonian.
 Rift phases occurred in the late Paleozoic and early Mesozoic which allowed the opening of the NE Atlantic.
 Differential uplift occurred in the late Paleogene and Neogene.
 The geology of the Southern North Sea basin has a complex history of basinal subsidence that had occurred in the Paleozoic, Mesozoic, and Cenozoic.
 Uplift events occurred which were then followed by crustal extension which allowed rocks to become folded and faulted late in the Paleozoic.
 Tectonic movements allowed for halokinesis to occur with more uplift in the Mesozoic followed by a major phase of inversion occurred in the Cenozoic affecting many basins in NW Europe.
 The overall saucer-shaped geometry of the southern North Sea Basin indicates that the major faults have not been actively controlling sediment distribution.