<<

TRANSACTIONS ON SCIENCE AND TECHNOLOGY thesubduction zones tobecome reheated andeventua and sideways turns rock cooledplastic causingthe surface the toheat release theylithosphere, of basethe reachcellsconvection year. whentime,the longperiodcentimetersof 10a Over a about of slowpace th from heat bring that cells convection are asthenosphere earth. theofearth.Withininteriortheofshellplastic Asthenosphereandbrittlethe rigid thehot, theis ea to relativesurfaces earth’s the across move that plates of dozen a into divided is earth the of layer rigid outer 1 sciencesince earth of study revolutionizedthe has theory tectonicPlate Introduction Seismicpotential assessment zoning,GM Tectonicearthquake, Seismic Arc andTrench System, Keywords: Online: Inpress: Accepted: Revised: Received: moves parallel to the earth’smovesmovement,attheparallelearthtoandforthdescendinto theyback Insurface. back Plate Tectonics SeismicActivities and in *Correspondingauthor: 1April 2016 Kao 25December 2015 8 January8 2016

27Novembe 7 January7 2016 ( hohr hs ltsbsclysprt ihshr n shnshr.Ltopee is Lithosphere asthenosphere. and lithosphere separate basically plates These other. ch

1,1 YuanUniversity, ) model, Cheng

r2015

,

2016.

[email protected] aaa ad iaga wti te et ee yas (2015 disaster red years seven , next , the within , , and Lahad in potential earthquake high be will there Additionally, occur. to ofearthquakes heavy to pointmoderate for possibility critical a factor trigger reached any If energy. have seismic accumulating Sea Celebes and that showsSandakan, result The earthquakes. future of zones potential seismic eight ofmodel uses study s eight into divided is area method, zoning seismic presen The zone. (M earthquakes seismic the of southeast years. majorThe earthquake affected isSabah area from the northwesttothe Sabah M two to leads which , North plates, small of collision the by influenced hand, other the on for As earthquake. which the by caused tsunami the by or deaths missing thousand ninety and hundred two than more to leading 2004, in i one M9.0 the is earthquakebigparticular One earthquakes. System Sunda of seismic ac and tectonic the on impact overall an has which system Trench and Arc Luzon Sunda the of southern westernand themainly byinfluencedSundais Cenozoic,Platethe the since early Su the the into subducted byis which influenced Plate, Sea mainlyChina structuralSouth is it the formed; ago, already years is million Sabah of 1.6 geology was which Pliocene the since Ever tsbA a ct r

1821 Zhongshan1821 Road Transactionson Science and Technology, Kuei tee s cmlt rcr o erhuk ctlg o mr ta 40 than more for catalog earthquake of record complete a is there , Sabah AreaSabah ≧ is

7 earthquakes (1996 M7.9 and 1999 M7.1) in the 20 the in M7.1) 1999 and M7.9 (1996 earthquakes 7 s locate Gr - ne h Quaternary the ince Jav - two predictive models, GM (1,1) model and GM (1,1) Verhuls (1,1) GM and model (1,1) GM models, predictive two uctionis needed. hsiang CHENGhsiang ey Forecasting theory in Grey System Theory, to evaluate these evaluate toTheory, System Grey theory in Forecasting ey

a tivity of . tivitySunda of

d ≧ r ad rnh ytm ad f uo Ac n Trench and Arc Luzon of and System, Trench and Arc

in residual arc, the impact of tectonic earthquake is trivial; is earthquake tectonic ofimpact the arc, residual in 3.7) occurred in Sabah area Sabah in occurred 3.7) the which belongs to the back the to belongs which Sea Celebes the

- Java Arc and Trench system, and the eastern side of side eastern the and system, Trench and Arc Java ; llydrives movements.the plate Tel: ,

LuzhuDistrict

886 e earth’s interior out the surface in a very a in surface the out interior earth’se ,

hc cue ay ag ad frequent and large many cause which - 7

D - * 6077750 espiteincreasingthetectonic activities

, 3

Kaohsiung,. (1), s suy s ae o te 66 the on based is study t 9th ; ; Fax:

since 1974. With the use of of use the With 1974. since 47 century. It describes the describescentury. It -

appears, there is a high high a is there appears, 58 886

nda Plate. Plate. nda

- eismic zones. The zones. eismic 7 - - 02. Possible 2022). n Indian OceanIndian n 6077762 th -

arc basin is basin arc century.

However, island

In In t

TRANSACTIONS ON SCIENCE AND TECHNOLOGY ng arc island, making the occurrence of multiple M7 shallow earthquakes. As for the eastern district easternthe for Asearthquakes. shallow multipleM7 of occurrence making the island, arc ng Bayan intectonic active the influencedby also is It Trench. Sulawesi Northof south the in collision back the to belongs which Sea Celebes The NorthSulawesi Plate residualof Borneoarc the State, influence of tectonicearthquake minimal.is incr is back of SeaSuluandCelebesSea earthquakes shallowin considerableM7 ofnumber a earthquakes anddeep seriesof causing a Plate, direct northwest the on is Plate Sea Philippine The Luzon Arcand TrenchSystem example. fore in locate which islands Sunda Lesser whic Plate Sunda the beneath the years, recent In Sunda Platetectonic s nextseven(2015years KudaTawau,Datu, Lahad in potentialearthquake high be highmoderatethere appears, earthquakesisa heavypossibilityoccur. for toto Additionally,willthere C and earthquakes(M 66 the on based isTheory.evaluation System TheGrey in models predictive two usingevaluated are are inSabah activitiesseismic the studytoworld the around agencies related and government local the from attentionsenormous drawn has news The ( Malaysiarecordedinearthquakes strongestofone seconds, was 30 for lasted rocks,energythe isreleased andeventually causingearthquake. the of threshold the exceeds it when and collision the during plates both in up builds stress Rather, other each past glide simply cannot plates the friction, of Because motion. horizontal in other each passed slide plates where are boundaries Transform magma. molten from sourced crustal new with t where are boundaries Divergentother. each within together or crust, continental and crust oceanic between subduction occur can form collision This tozones. colliding are plates tectonic two where are boundaries Convergent transform. Recently, an earthquake struck Ranau, Sabah with a magnitude of 6.0 on 5 on 6.0 of magnitude a with Sabah Ranau, struck earthquake an Recently, conver namely boundaries plate of kinds three are there section, cross In elebes Sea have reached a critical point of accumulating seismic energy. If any trigger factor trigger any If energy. seismic accumulating of point critical a reached have Sea elebes - easing but also is enhancing. However, concerning these two subduction zones to the same same the to zones subduction two these concerning However, enhancing. is also but easing Jav

a

Arcand TrenchSystem ≧ etting 3.7) occurred in Sabah areas since1974 areas Sabah inoccurred 3.7) Cheng (

MoluccaPlateSea - 2022). , -

utain lt i t te ot o Sunda of north the to is Plate Australian 2016.

h causes the increasing seismic activity in the Sunda Strait and the the and Strait Sunda the in activity seismic increasing the causes h ISSN2289

Transactionson Science and Technology, - arc basin. It appears that the tectonic and seismic activity not only notonly theseismic appears basin.that Itactivity tectonic and arc

wo tectonic plates are moving apart to create a space filled filled space a create to apart moving are plates tectonic wo - ) 8786. -

arc basin. The M9 earthquake in 2004 was one particular particular one was 2004 inearthquake M9 The basin. arc - http://transectscience.org/ arc a. In this work, potential zones of future earthquakesfuture of zonespotentialwork, thisIn a.

ion underneath from the trench to Sunda Sunda to trench Manila the from underneath ion ai i ifune bcue f h sal plate small the of because influenced is basin . t, Ranau, Tarakan and Sitangkai within the within SitangkaiTarakan Ranau,and t, ,Semporna that shows result The

- Java Trench and is subducted subducted is and Trench Java

3 (1), 47

- Earthquake Track,

58 th et dvret and divergent gent,

June 2015, June

which 2015 48 )

. .

TRANSACTIONS ON SCIENCE AND TECHNOLOGY (MS, southeast the in plates small four the by and boundaryPlate Sunda the on TrenchManila and Trench distributiontheir of showed were boundaries TectonicPlateSunda environment be can concerned Figure by 1. S of abah State, the near and far of epicenter will cause a number of damages to a certain extent. extent. certain a to damages of number a cause will epicenter of far and near the State, abah ic 17, h 2 pee o M. t 9 to M7.5 of pieces 26 the 1973, Since BS, TI andshownareBH) Figure2 : Majorearthquakes since which1973 occurred in Cheng Figurel: ,

2016.

ISSN2289 TectonicplateSunda diagram.

Transactionson Science and Technology, inFigure 3. - 8786.

( in Figure 2 Figure in USGS, 2015 USGS, 0 atqae ocre i te etnc ud Plate Sunda tectonic the in occurred earthquakes .0 http://transectscience.org/ .

The tectonic earthquakes induced by Sunda inducedby earthquakes tectonic The )

( W

TectonicSunda Plate boundaries ikipedia

3 (1), , 2015 , 47 -

58 )

49

TRANSACTIONS ON SCIENCE AND TECHNOLOGY schemeoffrom Sabah area Ego the as South the and Plate), Sea (Banda influenced movementby important the in Norththe Sulawesi (Molucca Sea Plate), Souththe Sulawesi Simons from data GPS the to According ArcBorneoThe

Figure3 :

Thetectonicearthquakes inPlate Sunda Cheng Figure4: ,

2016.

ISSN2289 Sundalandgeodynamic settings (Sapin

et al et Transactionson Science and Technology, ., (2006)., - 8786. t al. et is http://transectscience.org/ also

20) te ono area Borneo the (2007), shownin Figure 4 shown 4 Figure

( ScientificMalaysian, 2015

anotherdiagram .

T

et al et

3 he GPS motion and structural structural and motion GPS he (1), ., s 47

2013 slow movement be be may movement slow - inFigure 5

58 ).

) .

.

50

TRANSACTIONS ON SCIENCE AND TECHNOLOGY occurredfrom into2015 1974 depicted asSabah area, inFigure 6. M of pieces 66 the record to used is method zoning seismic The districtearthquakesThe of inSabah Data No 16 15 14 13 12 11 10 9 8 7 6 5 4 3 2 1

2008 2008 2009 2010 2012 2013 2014 2014 2014 2015 2015 2015 2015 2015 2015 2015 Year Figure5

Date Cheng 18 28 21 25 24 12 23 19 8 26 9 4 1 5 4 6 - : ------Nov - - - - Apr Sep Feb - Jun Jun Jun May May - Aug month Feb NWBorneo motion GPS scheme andstructural Oct Jun Jun Jan Jul ,

2016.

ISSN2289 Table

Transactionson Science and Technology, 00:51 06:26 04:49 19:43 16:44 19:23 11:35 05:40 20:07 17:19 01:31 23:15 05:45 18:29 09:32 16:10 Time

1:

Earthquakecatalogsinarea Sabah - 4.838, 118.7134.838, 118.1734.598, 11 7.191, 118.3685.370, 118.3214.786, 117.5612.984, 116.5896.157, 117.2477.194, 117.6033.594, 119.7614.624, 119.8446.089, 116.5295.979, 116.6085.956, 116.6516.182, 116.6066.159, 116.8686.224, 8786. Epicenter http://transectscience.org/ 7.115

Depth (km) 27 10 35 54 39 16 17 14 43 11 24 10 10 11 15 15

3.7 earthquakes (see as Table 1) Table as (see earthquakes 3.7

3 Magnitude

(1), ( Ego (M)

4.5 5.0 4.5 4.2 4.6 4.9 4.7 4. 4.4 5.5 5.6 6.0 4.5 5.3 4.5 4.6 47 6 et al et

-

58

., 20

Lahad Lahad Semporna 06). Sitangkai Tarakan Tarakan District Tawau Ranau Ranau Ranau Ranau Ranau Ranau Kudat Kudat

Jolo

Datu Datu

51

TRANSACTIONS ON SCIENCE AND TECHNOLOGY 39 38 37 36 35 34 33 32 31 30 29 28 27 26 25 24 23 22 21 20 19 18 17 54 53 52 51 50 49 48 47 46 45 44 43 42 41 40

1996 1999 2001 2 2003 2005 2005 2006 2006 2007 2008 1979 1980 1981 1981 1982 1983 1984 1984 1988 1989 1989 1989 1991 1991 1991 1991 1991 1992 1992 1992 1994 1994 1994 1995 1995 1996 1996 002

Cheng 30 24 26 26 26 26 23 25 27 11 26 22 14 25 14 22 13 22 28 23 23 30 10 2 3 6 4 31 8 6 9 7 5 7 9 1 4 4 ------Nov Aug - - - Mar Mar Dec Dec Dec - - Apr - Feb Feb - Oct May May May May May May Jan - May Nov Aug Nov Aug Jul Jul Mar M Dec Dec Apr Feb Feb Sep Oct Oct Jun Jan Jul ,

ar 2016.

ISSN2289

Transactionson Science and Technology, 02:01 15: 20:34 13:18 14:06 14:00 19:24 00:28 19:29 22:44 00:39 14:56 17:06 18:32 20:24 15:58 07:02 10:59 11:14 11:16 07:15 00:39 18:19 22:33 01:43 18:27 08:30 18:43 06:21 08:05 22:42 12:42 08:52 16:41 01:03 18:44 19:58 18:09 11

- 5.768, 119.3245.768, 120.8441.967, 118.2262.690, 117.1506.340, 119.9310.729, 119.6095.208, 118.6054.894, 121.9375.397, 117.4668.023, 117.0527.225, 118.7593.694, 117.7096.256, 115.6204.329, 117.8106.121, 117.3986.041, 119.3165.710, 116.5084.205, 6.886, 117.0046.886, 117.9576.519, 117.3193.796, 118.4774.760, 118.3874.895, 118.8623.835, 118.3875.203, 118.6004.108, 117.8595.753, 118.0894.560, 117.8434.265, 117.6743.455, 6.130 ,117.168 116.7465.865, 116.7485.718, 116.8155.869, 4.636 114.5465.415, 118.0494.579, 118.4544.976, 118.6435.099, 8786. ,118.256 http://transectscience.org/

27 38 16 33 24 33 33 33 33 33 33 19 24 70 10 48 10 33 51 57 39 33 57 50 33 79 24 32 10 33 33 33 18 33 40 50 10 55

3 (1), 5. 5.7 6.1 4.1 7.9 4.4 4.4 7.1 5.5 5.1 4.9 5.3 4.5 4.0 4.5 5.2 4.1 4.5 5.1 4.8 5.4 4.5 5.0 5.6 4.5 5.1 3.7 4.4 3.7 4.6 5.1 4.7 5.1 4.5 5.2 4.3 4.6 5.7 47 5

-

58

Lahad Lahad Lahad Lahad Lahad Gorontalo Semporna Semporna Semporna Semporna Semporna Sandakan Sandakan Sandakan Sandakan Sitangkai Sitangka Sitangkai Limbang Tarakan Tarakan Tarakan Tawau Tawau Tawau Ranau Ranau Ranau Ranau Ranau Ranau Kudat Kudat Pulot

Palu Seit Datu Datu Datu Datu Datu

i

52

TRANSACTIONS ON SCIENCE AND TECHNOLOGY

66 65 64 63 62 61 60 59 58 57 56 55

1976 1976 1976 1976 1976 1976 1976 1976 1976 1976 1976 1974 Figure6

:

Theseismic epicenter distribution diagram from into2015 1974 Sabah area. Cheng 14 12 18 18 26 26 25 26 26 26 26 26 ------Aug Nov Sep Jun Jul Jul Jul Jul Jul Jul Jul Jul ,

2016.

ISSN2289

Transactionson Science and Technology, 09:43 13:12 11:10 07:54 22:13 18:40 14:03 02:56 03:03 05:35 08:36 08:49

- 2.316, 121.1292.316, 119.7716.041, 118.2875.092, 118.3084.956, 118.3855.062, 118.5944.986, 118.0524.904, 118.3424.894, 118.5504.994, 118.4.592, 118.4214.714, 118.0334.639, 8786. http://transectscience.org/

160

54 33 33 33 33 33 33 33 33 33 36 33

3 (1), 5.8 4.5 5.3 6.2 5.3 5.2 5.3 5.3 5.1 4.5 5.1 5.0 47

-

58

Lahad Lahad Lahad Lahad Lahad Lahad Lahad G Semporna Tawau Tawau orontalo

Jolo Datu Datu Datu Datu Datu Datu Datu

53

TRANSACTIONS ON SCIENCE AND TECHNOLOGY

54 24 14 9 No. TableintoSabah,summarize1 eightinto earthqu of pieces 60 these use we zoning, seismic on Based Futureseismicpotentialassessment inSabah area Therecords60 eight of the seismic zonesshownare in No. 42 41 40 39 30 19 10

5 4 3 2 1 8 7 6 5 4 3 2 1 No.

1979 2002 2009 2014 Year 2015 2015 2015 2015 Year 1991 1991 1991 1991 1995 2006 2014 2015 Sitangkai Tarakan Tawau Lahad Sandakan Kudat Rana District CollisionZone

Date u Date

Datu

30 24 26 26 26 26 11 7 4 28 12 23

26

1 4 6 - - - - - month - - Apr - - Sep Cheng - - - - - May month - - - Feb Oct Jun Jun May May May May - Aug Sep Jun Jun Jul

Table2 , Quake no.Quake

2016.

14:06 01:03 04:49 05:40 Time 07:02 10:59 11:14 11:16 06:21 15:11 11:35 23:15 05:45 18:29 09:32 16:10 Time 12 10 17 ISSN2289 4 4 5 4 4 Table3: Table

Transactionson Science and Technology,

:

Seismiczoning andrange statisticstable

4 6.886, 117.0046.886, 117.0527.225, 117.1157.191, 117.2477.194, Epicenter : 6.113, 117.1686.113, 5.86 116.7485.718, 116.8155.869, 117.1506.340, 117.3986.041, 6.157, 116.5295.979, 116.6085.956, 116.6516.182, 116.6066.159, 116.8686.224, Epicenter

M maxM

- Ranau Ranau areaearthquakes list Kudatareaearthquakes list 8786. differentdistrictsfollowsas inTable 3 M7.9 M5.5 M6.1 M5.0 M6.2 M5.3 M5.1 M6.0 5,116.746 116.589 http://transectscience.org/

Longitu 120.0~122.0 119.3~119.8 117.3~118.3 117.8~118.9 118.0~118.9 117.5~118.0 116.8~117.4 116.4~117.4

T

able Depth Depth

2 de . ake catalog from the upper section of of section upper the from catalog ake

33 33 35 14 33 33 33 18 33 10 17 10 10 11 15 15 (

° (km) )

(km)

3

Latitude

(1), 0.5~5.5 4.6~5.8 2.6~3.8 3.6~4.7 4.7~5.5 5.5~6.6 6.6~7.4 5.5~6.4 Magnitude Magnitude

47 -

58

4.6 5.1 4.7 5.1 4.1 4.5 4.7 6.0 4.5 5.3 4.5 4.6 - (

4.5 5.1 4.5 4.6 °

10. 10. )

(M)

(M) Area 200*500 100*120 110*110

50*120 50*110 100*90 90*80 60*80

District (km District Ranau Ranau Ranau Ranau Ranau Ranau Ranau Ranau Ranau Ranau Ranau Ranau

Kudat Kudat Kudat Kudat

2

)

54

TRANSACTIONS ON SCIENCE AND TECHNOLOGY

13 12 No 64 63 62 61 60 59 58 56 51 50 48 35 34 27 16 52 43 31 11 8 No 53 46 22 20 No.

1976 1976 1976 1976 1976 1976 1976 1976 1981 1982 1984 1992 1994 1996 2008 2010 2012 Year 1981 1989 1995 2013 2014 Year 1980 1988 2005 2006 Year

Date Date Date 28 14 26 21 14 25 2 25 26 26 26 26 26 26 6 9 4 - - - - 23 8 6 9 - 14 9 22 5 ------23 Nov month Dec Apr ------May - Aug Nov Aug Mar Jul - Dec - - - - Jul Jul Jul Jul Jul Jul Jul month Nov Mar Dec - Oct Jun - - - month Cheng - May Dec Apr Oct

,

2016. 14:03 02:56 03:03 05:35 08:36 08:49 09:43 11:10 00:28 19:29 00:39 22:33 01:43 12:42 00:51 19:43 16:44 Time Table 19:24 15:58 18:43 19:23 20:07 Time 17:06 19:58 02:01 Time 14:00 Table Tabl ISSN2289

Transactionson Science and Technology,

6

e

5:

: 5.092, 118.2875.092, 118.3084.956, 118.3855.062, 118.5944.986, 118.4.904, 118.3424.894, 118.5504.994, 118.4214.714, 118.4774.760, 118.3874.895, 118.3875.203, 118.4544.976, 118.6435.099, 4.894 118.7134.838, 118.3685.370, 118.3214.786, Epicenter 7:

LahadDa

5.753, 117.8595.753, 117.7096.256, 117.8106.121, Epicenter 6.519, 117.9576.519, Epicenter 3.796, 117.3193.796, 117.6743.455, 118.2262.690, 117.5612.984, 117.6033.594, Sandakanearthquakes area list

Tarakanareaearthquakes list - 8786. ,118.605 http://transectscience.org/ t 052

u areaearthquakes list

Depth(km) Depth(km) Depth 33 50 10 55 33 27 54 39 33 33 33 33 33 33 33 36 39 51 79 19 70 57 10 16 16 43

(km)

3

Magnitude(M) (1), Magnitude(M) Magnitude 47 4.5 5.6 4.6 5.7 4.4 4.5 4.2 4.6 5.3 6.2 5.3 5.2 5.3 5.3 5.1 5.1 5.4 -

5.1 5.1 5.3 4.0 58

4.8 3.7 6.1 4.9 4.4

(M)

Lahad Lahad Lahad Lahad Lahad Semporna Lahad Lahad District Lahad Lahad Lahad Lahad Lahad Lahad Lahad Semporna Semporna

Sandakan Sandakan Sandakan Tarakan Tarakan Tara Tarakan Tarakan District

Datu Datu Datu Datu Datu Datu Datu Datu Datu Datu Datu Datu Datu Datu

kan

55

TRANSACTIONS ON SCIENCE AND TECHNOLOGY

and(1.1) Verhulst,GM the M next GM model, prediction gray two the uses which study present the on based However, 2040. around earthquake M5.5 another be will there that means which years 25 is area Ranau of cycle earthquake Tongk to According AreaRanau thestudy and area, Sabah in zones differentseismic at potential seismic future assessingof method the use We Results& 57 55 45 49 47 44 38 36 23 15 No 66 32 29 26 No 33 28 18 7 No

1976 1976 1989 1983 1984 1989 1991 1992 2003 2008 Year 1974 1994 1996 1999 Year 1994 1996 2007 2015 Year canget analytical resultseach infollows:as area

d

iscussion

Date Date Date 24 18 25 22 18 13 12 3 26 5 4 8 4 1 - 27 - - - 23 - - - - 19 - - - Aug - - - month 7 - Feb Mar May month - May Dec Aug Mar Jul Jan Sep Feb Nov Jul - Cheng - - - Feb - u month Nov Oct Jan

l’s estimation ( estimation l’s

,

2016.

18:44 06:26 Time 13:12 07:54 18:32 22:44 14:56 20:24 07:15 18:19 22:13 08:30 08:05 08:52 Time Table 18:27 22:42 20:34 17:19 Time Table ISSN2289 Table

Transactionson Science and Technology,

10

5.0earthquake willoccurredbe around2019 9: Tongkul, Tongkul,

4.592, 118.1604.592, 118.0334.639, 118.0894.560, 118.8623.835, 4.108, 117.8434.265, 118.2564.636, 118.0494.579, 118.7593.694, 118.1734.598, Epicenter 8: : 2.316, 121.1292.316, 120.8441.967, 119.9310.729, 121.9375.397, Epicenter

5.768, 119.3245.768, 119.6095.208, 119.3165.710, 119.7614.624, Epicenter Sitangkai CollisionZoneearthquakes list

Tawau areaearthquakesTawau list - 8786.

118.600 http://transectscience.org/ 2015) from the the from 2015)

area earthquakes area list

Depth(km) Depth(km)

Depth 33 33 24 57 33 32 33 50 33 10 54 38 2 33 48 11 27 33 Universiti Sabah Malaysia Universiti 4

(km)

3

(1), Magnitude(M) Magnitude Magnitude(M) 47 4.5 5.0 3.7 5.0 4.5 4.4 4.5 4.3 4.9 5.0 - 5.2 5.5 5.5 4.4

5.8 5.7 7.9 7.1 58 -

2020 in2020 Ranau area.

(M)

Tawau Tawau Tawau Semporna Semporna Tawau Semporna Tawau Semporna Sitangkai Sitangkai District Sitangkai Sitangkai , the M the , Gorontalo Gorontalo Palu Seit District

≧ 56

5

TRANSACTIONS ON SCIENCE AND TECHNOLOGY Table11 as area Sabah in assessment potential seismic future get can study present the State, Sabah occur M Theoretically, estimation. model (1,1) GM the using earthquakes of range critical enteredthe now earthquakehas M≥6.0 nextthe Sea, Celebes the of Zone Collision the for As CelebesCollisionSea Zone occur will earthquake 5 M> around2020 next the area, Sitangkai of estimation model (1,1) GM the on Based Area Sitangkai Butif basedon the 2019 around be will area Tawau in earthquake next the estimation, model (1,1) GM on Based Area Tarakan thecriticalinpoint, theory, anearthquake toisveryoccur likely any at time. area Tawau the in aroundoccur2017 will earthquake An TawauArea earthquakenextthe depthat of will 33kmaround occur2021 2016 earliestaround occur willearthquake another not, or in1992 earthqu M4.6 the ignore to whether estimation, model (1,1) GM on Based Lahad AearthquakeM5 whosedepthkmis70 inwilloccur inSandakan area 2015. AreaSandakan 2020 ea two next the estimation, model (1,1) GM on Based KudatArea -

2021 respectivelyinKudatarea. at any time in this region. this in anytime at Datu :

- Area 2021. As forthe2021. estimationof Verhulstmodel,GM datethew

GM(1,1) Cheng ,

2016.

Verhulstmodel, earthquakenextthe will occur around 2021 ISSN2289

Transactionson Science and Technology, If we take the above eight sections of future potential earthquakes in potential future of sections eight above the take we If

- 8786. http://transectscience.org/ tqae wl ocr rud 2017 around occur will rthquakes . But the Semporna area has alreadyreachedhas area Sempornathe But . - 2022. - 2017 and slowest in 2026. And the the And 2026. in slowest and 2017

3 (1), illbetwoearlier. years 47

k tadph f1 km 10 of depth a at ake -

58 ≧ 6.0 earthquake will will earthquake 6.0

-

2022. 2022. - 2018 and and 2018 shown in in shown

-

2020.

57

TRANSACTIONS ON SCIENCE AND TECHNOLOGY [8] [7] [6] [5] [4] [3] [2] [1] References included. Sitangkai,Lahad Tarakan, Ranau, Kadat, as such areas other ( regions, years seven next the in State Sabah in areas potential Lahad are areas potentials seismic higher Another earthquakes. induce and dislocation fault the cause will it place, take factors trigger the as long As energy. strain enough accumulated currently have areas three These Sea. Celebes the and Semporna, (2015 years three next the in State Sabah in region potential seismic high The Conclusion

2015. Wikipedia. December2015. boundaries Plate (NEIC). Tectonic Center Information Earthquake National USGS F. 2015. (http://www.thestar.com.my/news/nation/2015/06/07/sabah Tongkul. resolvingSundaland motionandboundaries. P. Morgan, S., Matheussen, A., D. Sarsito, F., J. W. Simons, asia/). Malaysian. (http://www.scientificmalaysian.com/project Scientific International Wedge Borneo NW the F., Sapin, Track. (http://earthquaketrack.com/p/malaysia/sabah/recent).Accesssed 18on December 2015. Earthquake TectostrainProject: structures andstrain field, Central South Chamot F., Ego,

Accesssed18on December 2015.

Hermawan ( 2015 , 12 11 10 9 8 7 6 5 4 3 2 1 No. 193

Cheng -

Rooke, N., Loevenbruck, A., Lorne, A., Pubellier, M., Rabaute, A. & Vigny, & A. Rabaute, M., Pubellier, A., Lorne, A., Loevenbruck, N., Rooke, ) (2), 549

Socquet, A., Vigny, C., Ambrosius, B. A. C., Haji Abu, S Abu,Haji C., A. Ambrosius,B. Vigny,C., Socquet,A., . ud Plate Sunda , I., Pubellier, M., Vigny, C. & Ringeubach, J. Ringeubach, & Vigny, M.,C. Pubellier, I., , 2 2 2 2 2 2 2 2 2 ~now ~now ~now Year , Table11 022 022 021 021 020 020 018 017 017

2016. ( - - 2015

556.

crustal a

ISSN2289 (

Transactionson Science and Technology, 2015 (

http://earthquake.usgs.gov/contactus/golden/neic.php ) 4.5 M5.0 Magnitude . 4.5 4.5 4.5 4.5 4.5 4.5 4.5 4.5 4.5 M

( : ( 2015

https://en.wikip Futureseismic potential inS ≧ ) ≦ ≦ ≦ ≦ ≦ ≦ ≦ ≦ ≦ ≦ . 6.0 - M M M M M M M M M M

) Erhuk gooy f otes Asia Southeast of geology Earthquake . cl gaiy ldn eiecd rm GPS. from evidenced gliding gravity scale -

≦ ≦ ≦ ≦ ≦ ≦ ≦ ≦ ≦ ≦ aa quake: Sabah 8786.

6.0 5.0 5.0 5.0 6.0 6.0 5.0 5.0 6.0 5.0 eet atqae er aa, Malaysia Sabah, Near Earthquake Recent

- & Geodesyand Gravity Tectonophysics

collab

(M) http://transectscience.org/ Spakman, W Spakman, edia.org/wiki/Sunda_Plate

- directory/1079/earthquake Datu ~33km ~33km ~33km 70km Depth

and Tawau. and 2015 - quake . -

( .East Unpublished report.

2015 (

(km) 2007 - 2022), in addition to the above five five above the to addition in 2022), - abah area abah ) geologist/). Accesssed on 18 December 18 on Accesssedgeologist/). . )

- gooits perspective geologist’s A Asia:Southeast in GPS ofdecade A . C. C. ao erhuks ic 1973 since earthquakes Major ( Lahad Tawau Kudat Sitangkai Tarakan Ranau Kudat Tawau Lahad CelebesSea Semporna Sandakan District

Datu

2013 3 According to the high seismic high the to According (1), ). ., Subarya, C., Promthong,C., Subarya, C., .,

, and Tawau areas are also are areas andTawau , ) 47 - convergenceon recent The . cese o 1 December 18 on Accesssed

geology

Datu Datu

-

,

58

- 112 2017) are Sandakan, are 2017) ).

epyia Journal Geophysical , B06420. , - cese o 18 on Accesssed of - southeast

C. C.

( - 2006 and 58 ) .