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In this paper the economic base model reflected in the Location Quotient (LQ) which features shift share analysis, useful to know the leading sectors in the city of Tangerang. A major aftershock (magnitude 7.1) can be seen at the closest stations starting just after the 200 minute mark. Based on the results using the Location Quotient, sector that has a LQ greater than one and a sector basis economy is the manufacturing sector with an average LQ of 1.06%, then trade, hotels and restaurants with an average of LQ 1.43 %, As well as Transport and Communication sector, with an average LQ of 1.59%. ^ “Jakarta Malls and Shopping Centers – luxury shopping in Jakarta, Indonesia”. This aftershock would be considered a major earthquake under ordinary circumstances, but is dwarfed by the mainshock. This study uses data of Gross Regional Domestic Product (GDP) City of Tangerang and Banten Province in 2001 until 2004. The largest amplitude signals are seismic surface waves that reach the antipode after about 100 minutes. Such data obtained from the secondary survey, by utilizing the available data the relevant agencies. The surface waves can be clearly seen to reinforce near the antipode (with the closest seismic stations in Ecuador), and to subsequently encircle the planet to return to the epicentral region after about 200 minutes. On October 31, 1945, Laskar Hitam kidnapped Otto Iskandardinata, Republic of Indonesia’s Minister of State. ^ “Condemned Communities: Forced Evictions in Jakarta” Human Rights Watch Sep 2006. The Andaman and Nicobar Islands appear to have shifted south-west by around 1.25 m (4.1 ft) and to have sunk by 1 m (3.28 ft).[32] In February 2005, the Royal Navy vessel HMS Scott surveyed the seabed around the earthquake zone, which varies in depth between 1,000 m and 5,000 m (3,300 ft and 16,500 ft). He persumably was murdered at Mauk beach, Tangerang on December 20, 1945. The survey, conducted using a high-resolution, multi-beam sonar system, revealed that the earthquake had made a huge impact on the topography of the seabed.

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This movement later became a part of DI/TII rebel group. Early speculation was that some of the smaller islands south-west of Sumatra, which is on the Burma Plate (the southern regions are on the Sunda Plate), might have moved south-west by up to 36 m (118 ft), but more accurate data released more than a month after the earthquake found the movement to be about 20 cm (7.9 in).[31] Since movement was vertical as well as lateral, some coastal areas may have been moved to below sea level.

Many international corporations have plants in the city. These volatiles rise into the overlying plate causing partial melting and the formation of magma.

Tangerang tends to be hot and humid, with little in way of trees or geographical features. The rising magma intrudes into the crust above and exits the Earth’s crust through volcanoes in the form of a volcanic arc.

Firstly, Jakarta – Merak highway which have three different exits points to Tangerang city. This energy is equivalent to over 1502 times that of the Hiroshima atomic bomb, but less than that of Tsar Bomba, the largest nuclear weapon ever detonated. International Association of Classical Archaeology (AIAC).

Secondly, Bumi Serpong Damai – Jakarta Outer Ringroad highway providing direct tol access from Tangerang, Jakarta, Bekasi, and Bogor. However, this is but a tiny fraction of the total work done MW (and thus energy) by this quake, 4.0×1022 joules (4.0×1029 ergs),[25] the vast majority underground.

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