Zon Kota Kinabalu Zon Tawau Zon Sandakan Zon Keningau

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Zon Kota Kinabalu Zon Tawau Zon Sandakan Zon Keningau

ZON KOTA KINABALU ZON TAWAU ZON SANDAKAN ZON PANTAI BARAT ZON KENINGAU UTARA ZON BEAUFORT ZON KOTA KINABALU ZON BEAUFORT THE YI YING-PERGIGIAN BEAUFORT BASRIAH BINTI JAPAR - HQE MAJANAH BINTI AB.HAMID – PERGIGIAN JUNAIDAH ABD.RAHIM HEE- K.KINABALU MAISALAMAH BT.ALIAS-PERGIGIAN PKK BEAUFORT PENAMPANG NURAH BINTI YUNUS – GEO ALLEN GEORGE - HMBP H.BEAUFORT DIVIKI M.S TIARASON - HWKKS KATHERINE YONG - HWKKS HANA FARIZA BINTI HADINAH@INAH BINTI BASINAU – HQE 2 MUHAMAD YUNUS – RUSIDAH BT.EJIB - PERGIGIAN K.KINABALU H.KUALA PENYU RITA EBIN – H.TUARAN DATU ASRIN BIN DATU D.T RAYA – H.TUARAN HAYATI BINTI MUMIN – CHUPIA GUTING – PKK TUARAN H.KUALA PENYU SALMAH BINTI JURI – H.KOTA BELUD CONNIE MICHAEL- MOHD FAKHRI BIN SAIMAN – H.RANAU DEIDRE JOANES LUNG – H.RANAU H.SIPITANG JUNAIDAH BINTI DIMAN- PERGIGIAN K/BELUD DOROTHIA ANGKUI- MOHD RIDUAN ABD RASHID - HWKKS H.BEAUFORT JUSTINA SALUNDA - HQE MARIA ONJIMI – H.TUARAN ZON KENINGAU ZON PBU DR. JUDITH LINUS LOJIKIP-PERGIGIAN TN.HJ. KHAIRUN NAIM JAILUN B. ABDULLAH- KENINGAU H.PITAS SITTI HAMIDA BINTI RAMLI-PKK MOHD. AMIR BIN MOHD NOR KENINGAU – H.KOTA MARUDU NUR FARHANA YVONNE TAIPAH@IPAH BTE LAKASA – ROBERT – H.KENINGAU H.PITAS NORAFIZAH BTE JAMILAH – WENNIE LEONG-PKK KUDAT H.KENINGAU NORAFSHANEH BT. ABD AHMAD ABDULLAH – HAMID – HOSPITAL PITAS H.TAMBUNAN MASNI LIMPANGAN- H.TAMBUNAN ZON SANDAKAN ZON TAWAU RIDUAN NANANG –H.KINABATANGAN JUSMAN BIN HEDOH –H.TAWAU SATRIA BINTI ARSAD-PKK PATRICK CHONG YEN MING – SANDAKAN H.L/DATU LUCY PALISA-PERGIGIAN EDAWATI HAMSAH -PKK L/DATU SDKAN HALIMAH BINTI CHONGKENG – RINDA SUHANI BT.ABD H.TAWAU SHUKUR-PKK BELURAN EDEMIKE SUADIN – H.KINABATANGAN SHAFFIE SUAMIN-PKK KINABATANGAN MUHAMAD SARUL ABDUL MURAT - HDOK .

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Plate Tectonics and Seismic Activities in Sabah Area
Plate Tectonics and Seismic Activities in Sabah Area Kuei-hsiang CHENG* Kao Yuan University, 1821 Zhongshan Road, Luzhu District, Kaohsiung, Taiwan. *Corresponding author: [email protected]; Tel: 886-7-6077750; Fax: 886-7-6077762 A b s t r a c t Received: 27 November 2015 Ever since the Pliocene which was 1.6 million years ago, the structural Revised: 25 December 2015 geology of Sabah is already formed; it is mainly influenced by the early Accepted: 7 January 2016 South China Sea Plate, which is subducted into the Sunda Plate. However, In press: 8 January 2016 since the Cenozoic, the Sunda Plate is mainly influenced by the western and Online: 1 April 2016 southern of the Sunda-Java Arc and Trench system, and the eastern side of Luzon Arc and Trench system which has an overall impact on the tectonic Keywords: and seismic activity of Sunda plate. Despite the increasing tectonic activities Arc and Trench System, of Sunda-Java Arc and Trench System, and of Luzon Arc and Trench Tectonic earthquake, Seismic System since the Quaternary, which cause many large and frequent zoning, GM（1,1）model, earthquakes. One particular big earthquake is the M9.0 one in Indian Ocean Seismic potential assessment in 2004, leading to more than two hundred and ninety thousand deaths or missing by the tsunami caused by the earthquake. As for Borneo island which is located in residual arc, the impact of tectonic earthquake is trivial; on the other hand, the Celebes Sea which belongs to the back-arc basin is influenced by the collision of small plates, North Sulawesi, which leads to two M≧7 earthquakes (1996 M7.9 and 1999 M7.1) in the 20th century.
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