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This is a shortened version of the eleventh chapter of the ICD-9: Complications of Pregnancy, Childbirth, and the Puerperium.It covers ICD codes 630 to 679.The full chapter can be found on pages 355 to 378 of Volume 1, which contains all (sub)categories of the ICD-9.
The Baribis Fault (Indonesian: Sesar Baribis) is a geological feature located in the northern part of Java. [1] This fault, estimated to be 100 kilometers (62 miles) long, stretches from Purwakarta to Lebak Regency [2] and is a threat to the Jakarta metropolitan area because the fault is partially located within the metropolitan area itself.
Danny Hilman Natawidjaja is an Indonesian geologist specializing in earthquake geology [1] and geotectonics at the Indonesian Institute of Sciences (LIPI) Research Center for Geotechnology.
The moment tensor solution is displayed graphically using a so-called beachball diagram. The pattern of energy radiated during an earthquake with a single direction of motion on a single fault plane may be modelled as a double couple, which is described mathematically as a special case of a second order tensor (similar to those for stress and strain) known as the moment tensor.
The Lembang Fault (Indonesian: Sesar Lembang) is an active fault located 10 km north of the city of Bandung on the Indonesian island of Java.This sinistral slip fault is estimated to measure 29 km in length. [1]
Teluk Dalam (also written as Telukdalam) is a town and district in the South Nias Regency, North Sumatra province, Indonesia. Following the splitting off of parts of the original district to form new districts, it is now mainly confined to the town, and its area is now 110.11 km 2 (42.51 sq mi).
Karawang (Kota Karawang or Karawang Kota) is the capital of the Karawang Regency of West Java, Indonesia.It is 32 miles east of Jakarta, and had a population of 307,880 at the 2020 Census, [2] spread over two districts of the regency - West Karawang and East Karawang.
The fault forms part of the boundary between two of the major crustal blocks that form the island, the North Sula Block and the Makassar Block.The current slip rate along the Palu-Koro Fault is estimated to be in the range 30 to 40 millimetres (1.2 to 1.6 in) per year, compared to a long term slip rate of 40 to 50 millimetres (1.6 to 2.0 in) per year over the last 5 million years.