ライフサイエンスコーパス: Sumatra

1 associated with future land use scenarios in Sumatra.

2 status given to the remaining peatswamps on Sumatra.

3 he living orang-utan (Pongo) from Borneo and Sumatra.

4 ) and limited to a localized area in Central Sumatra (1.6% of Indonesia): burning an estimated 163,33

5 Toba, Sumatra, 75,000 y ago, which produced voluminous ash dep

6 and southeast Asia, including the islands of Sumatra and Borneo in the Indonesian archipelago.

7 bes the southeast Asian great apes native to Sumatra and Borneo.

8 Longer-term records of airport visibility in Sumatra and Kalimantan show that 2015 ranked after 1997

9 r DNA from orang-utans from two locations in Sumatra and nine locations-representing four isolated po

10 land management on the Indonesian island of Sumatra and the sensitivity of this fire activity to int

11 the plate boundary offshore of northwestern Sumatra and the southern Nicobar islands.

12 d animals, than in the Sunda Region (Borneo, Sumatra, and Peninsular Malaysia), with a highly diverse

13 The 2004 Sumatra-Andaman and 2011 Tohoku-Oki earthquakes highligh

14 The human tragedy caused by the Sumatra-Andaman earthquake (moment magnitude 9.3) on 26

15 ic events, namely the 2004 magnitude (M) 9.1 Sumatra-Andaman earthquake and the earlier 1992 M = 7.3

16 The great Sumatra-Andaman earthquake and tsunami of 2004 was a dra

17 trength changes produced by the distant 2004 Sumatra-Andaman earthquake are especially important, as

18 of other great earthquakes indicate that the Sumatra-Andaman earthquake did indeed have a moment magn

19 Swedish survivors of tsunamis from the 2004 Sumatra-Andaman earthquake had increased risks of psychi

20 owing the massive loss of life caused by the Sumatra-Andaman earthquake in Indonesia and its tsunami,

21 The 26 December 2004 Sumatra-Andaman earthquake initiated slowly, with small

22 The disastrous Sumatra-Andaman earthquake of 26 December 2004 was one o

23 results reveal that Indonesia's devastating Sumatra-Andaman earthquake on 26 December 2004 was 2.5 t

24 as contiguous with that of the December 2004 Sumatra-Andaman earthquake, and is likely to have been s

25 of 9.0 was obtained several hours after the Sumatra-Andaman earthquake, but more recent, longer-peri

26 ccurring in the few years following the 2004 Sumatra-Andaman earthquake.

27 ty change induced by the great December 2004 Sumatra-Andaman earthquake.

28 edge of the 2005 rupture from the great 2004 Sumatra-Andaman rupture.

29 Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to

30 Shallow slip offshore Sumatra appears driven by diagenetic strengthening of de

31 The Toba supereruption in Sumatra, approximately 74 thousand years (ka) ago, was t

32 corded by continuous geodetic stations along Sumatra as the result of water- and stress-activated cre

33 c "supereruption" of the Mount Toba volcano (Sumatra) at approximately 74,000 y before present (B.P.)

34 ethods used to easily discriminate Siam from Sumatra balsam (also known as Benzoe sumatranus Indonesi

35 g of mammalian teeth, place modern humans in Sumatra between 73 and 63 ka.

36 of up to 15 meters occurred near Banda Aceh, Sumatra, but to the north, along the Nicobar and Andaman

37 The 2004 M = 9.2 Sumatra earthquake altered seismicity in the Andaman bac

38 bservations of the 2012 moment magnitude 8.6 Sumatra earthquake reveal unprecedented complexity of dy

39 ty over a large area associated with 3 major Sumatra earthquakes in 2004, 2005, and 2007.

40 We find ~80% of 2005-2009 Sumatra emissions are associated with degradation or lan

41 study area, we predict that 37-48% of future Sumatra emissions from land use change will occur in fue

42 as on the neighbouring, vertical strike-slip Sumatra fault, and find an increase in stress on both st

43 expanded the area of increased stress on the Sumatra fault.

44 We estimate Sumatra fire emissions from land use change and maintena

45 tracted from corals of the Mentawai islands, Sumatra, imply that this 700-kilometer-long section of t

46 p of the Sunda megathrust, offshore northern Sumatra, in March 2005.

47 d-based programs, a study was carried out in Sumatra, Indonesia, of the effect of food sources of bet

48 eflection profiles across the trench west of Sumatra, Indonesia, show differences across the boundary

49 egrees S-5 degrees N) and the region off the Sumatra-Java coast (SJC: 100 degrees E-110 degrees E, 13

50 h are located in Borneo (P. p. pygmaeus) and Sumatra (P. p. abelii), respectively.

51 sampled incoming sediments offshore northern Sumatra, revealing recent release of fresh water within

52 ed about 100-200 kilometres southwest of the Sumatra subduction zone.

53 neo (subspecies Pongo pygmaeus pygmaeus) and Sumatra (subspecies P. p. abelii).

54 aves from the 26 December 2004 earthquake in Sumatra swept across Alaska, they triggered an 11-minute

55 slab pull stresses as the plate underthrusts Sumatra to the northeast.

56 propagation patterns of the 26 December 2004 Sumatra tsunami were primarily determined by the orienta

57 the extent of the inundation in Banda Aceh, Sumatra, were combined with satellite imagery to quantif

58 econstructed rainfall changes over Northwest Sumatra (western IPWP, Indian Ocean) throughout the past

59 wider sampling of N. n. diardi in Borneo and Sumatra, would support reclassification of N. n. diardi