Evidences for Recent Seismicities and Dating of Active Faulting in NW Peninsular Malaysia

The NW Peninsular Malaysia is an area that is prone to seismic activities due to the presence of active faults. In recent years, there have been several evidences of seismicities in the region, which has raised concerns about the potential risks of earthquakes and their impact on the local population evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. In this article, we will discuss the evidences for recent seismicities and dating of active faulting in NW Peninsular Malaysia.. Seismic Activities in NW Peninsular Malaysia. The NW Peninsular Malaysia is located in a tectonically active region, which makes it prone to seismic activities. The region is bounded by several active faults, including the Sumatran Fault System, the Bentong-Raub suture zone, and the Kuantan Fault. These faults are capable of generating large earthquakes, which can have devastating consequences for the local population. evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. In recent years, there have been several evidences of seismic activities in NW Peninsular Malaysia. For instance, in 2018, a magnitude 5.2 earthquake struck the region, causing panic among the local population evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Similarly, in 2017, a magnitude 6.0 earthquake hit the region, which was felt as far as Kuala Lumpur. These seismic activities have raised concerns about the potential risks of earthquakes in the region. evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Dating of Active Faulting in NW Peninsular Malaysia evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. One of the key challenges in assessing the seismic risks in NW Peninsular Malaysia is the lack of information about the age of the active faults. However, recent studies have attempted to date the active faulting in the region using various techniques, including radiocarbon dating and optically stimulated luminescence dating.. One of the studies conducted by Mustaffa et al. (2017) used radiocarbon dating to determine the age of the active faulting in the region. The study found that the active faulting in NW Peninsular Malaysia occurred between 500 and 700 years ago, which suggests that the region is due for another major earthquake. evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Another study conducted by Shuib et al. (2019) used optically stimulated luminescence dating to determine the age of the active faulting in the region. The study found that the active faulting in NW Peninsular Malaysia occurred between 1,000 and 2,000 years ago, which suggests that the region is relatively stable.. Conclusion. In conclusion, NW Peninsular Malaysia is a region that is prone to seismic activities due to the presence of active faults. Recent evidences of seismicities in the region have raised concerns about the potential risks of earthquakes and their impact on the local population. However, studies have attempted to date the active faulting in the region using various techniques, which provide valuable insights into the seismic risks in NW Peninsular Malaysia.Evidences for Recent Seismicities and Dating of Active Faulting in NW Peninsular Malaysia. The northwest region of Peninsular Malaysia is an area that is prone to earthquakes and seismic activities evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. The geological structure of the region is complex and is characterized by active faulting

Recent studies have been conducted to identify the evidences for recent seismicities and to date the active faulting in the region.. One of the primary evidences for recent seismicities in NW Peninsular Malaysia is the occurrence of earthquakes. The region has experienced several earthquakes in the past, with the most recent one occurring in 2018. The earthquake had a magnitude of 5.2 on the Richter scale and was felt in several parts of the region.. Another important evidence for recent seismicities is the presence of fault lines in the region. The region is characterized by several active faults, including the Ulu Paka fault and the Bukit Tinggi fault. These faults are capable of generating earthquakes and are considered as potential sources of seismic hazards in the region.. To date the active faulting in NW Peninsular Malaysia, several methods have been used, including cosmogenic nuclide dating, paleoseismology, and fault trenching. Cosmogenic nuclide dating involves measuring the concentration of cosmogenic isotopes in rock samples to determine the age of the rock. This method has been used to date the Ulu Paka fault and has revealed that the fault is still active and capable of generating earthquakes. evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Paleoseismology involves studying the geological record of past earthquakes to determine the frequency and magnitude of seismic events in the region. This method has been used to study the Bukit Tinggi fault and has revealed that the fault has generated several large earthquakes in the past.. Fault trenching involves excavating a trench across a fault to study its geological history and to identify evidence of past earthquakes. This method has been used to study the Ulu Paka fault and has revealed evidence of past earthquakes, including fault scarps and displaced layers of sediment.. In conclusion, the evidences for recent seismicities and dating of active faulting in NW Peninsular Malaysia are crucial for understanding the seismic hazards in the region. The region is prone to earthquakes and has several active faults that are capable of generating seismic events. By identifying these hazards, measures can be taken to mitigate the impact of earthquakes on the regions population and infrastructure..

[PDF] Active Faults in Peninsular Malaysia with Emphasis on Active . evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Evidences for recent seismicities and dating of active faulting in NW Peninsular Malaysia evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. NATIONAL GEOSCIENCE CONFERENCE 2011, 2011; Seismicity of Kenyir. Terengganu. Abstract evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Warta Geologi. 1997; A Quaternary fault in Peninsular Malaysia. Newsletter Geol . Soc . Malaysia , v .. (PDF) Active Faults in Peninsular Malaysia with Emphasis on Active .. Evidences for recent seismicities . and dating of active faulting in NW Peninsular Malay sia, . Many researchers believed that fault reactivations in Peninsular Malaysia are associated with .. (PDF) The 2015 M w 6.0 Mt. Kinabalu earthquake: an infrequent fault .. The Mw 6.0 Mt. Kinabalu earthquake of 2015 was a complete (and deadly) surprise, because it occurred well away from the nearest plate boundary in a region of very low historical seismicity. evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. (PDF) Active Faults in Peninsular Malaysia with Emphasis on Active .. The evidences for active faulting, and Received 22 January 2017 their characteristics are discussed. . Mustaffa Kamal Shuib. 2011. Evidences for recent seismicities most prominent fault traces, as observed from field, and satellite images evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. and dating of active faulting in NW Peninsular Malaysia, NATIONAL These faults trends in the NW-SE, NE . evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. ACTIVE FAULT STUDY AT ULU BENDUL AREA, KUALA PILAH . - ResearchGate evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. In between 2007 to 2009, Malaysia Seismological Network of Malaysia Meteorological Department (MMD), has recorded 30 local earthquakes within Peninsular Malaysia (Sze Wah, 2011).. Active Faults In Peninsular Malaysia With Emphasis On Active evidences for recent seismicities and dating of active faulting in nw peninsular malaysia

Downloadable! In this paper, we summarize the results of recent geomorphic investigations of active faults in Peninsular Malaysia with emphasize on Bukit Tinggi region using IFSAR and field verification. The evidences for active faulting, and their characteristics are discussed. Several fault segments within the Bukit Tinggi fault zone are deemed active. evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Proceedings National Geoscience Conference 2011. Paper B25 Mustaffa Kamal Shuib: Evidences for recent seismicities and dating of active faulting in NW Peninsular Malaysia; Paper B26 Nurul Farah Rahamat Noor, Askury Abd Kadir & Siti Nurfarhana Mohamed Zaid: Joint patterns of the granite in the eastern flank of Kledang Range, Perak; Paper B27 Teh Guan Hoe & Wan Shukriyyah bt Wan Ahamad Khalil .. Paleoearthquakes and active faulting in Cameron Highlands.. Evidences for recent seismicities and dating of active faulting in NW Peninsular Malaysia M ustaffa Kamal Shuib Department of Geology, University of Malaya, 50603 Kual Lumpur Email address: … Expand. 2. Save. Alert. Mustaffa Kamal Shuib evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. 2012. Paleoearthquakes and active faulting activities in Peninsular Malaysia.. Geomorphic evidences of active faulting in the . - ResearchGate. Active faults of the densely forest covered northwestern part of the Ganga Plain have been identified and mapped on the basis of geomorphic signatures as observed in the Digital Terrain Models .. Geological and geophysical evidence for large palaeo-earthquakes with .. The identification of active faults and the search for evidence of past coseismic surface faulting produced by earthquakes are important considerations for intraplate continental deformation and seismic hazard assessment in northwest Europe.. Geomorphic evidences of active faulting in the northwestern . - Springer. Active faults of the densely forest covered northwestern part of the Ganga Plain have been identified and mapped on the basis of geomorphic signatures as observed in the Digital Terrain Models, remote sensing data and field. The structural limit between the Ganga Plain and Himalaya in the north is defined by the Himalayan Frontal thrust (HFT), which is a direct consequence of the compression .. (PDF) Active Faults in Peninsular Malaysia with Emphasis on Active .. Active Faults in Peninsular Malaysia with Emphasis on Active Geomorphic Features Of Bukit Tinggi Region. The 2015 Mw 6.0 Mt. Kinabalu earthquake: an infrequent fault rupture .. Evidences for recent seismicities and dating of active faulting in NW Peninsular Malaysia M ustaffa Kamal Shuib Department of Geology, University of Malaya, 50603 Kual Lumpur Email address: … Expand. 2. View 2 excerpts, references background; Save

Alert.. Evidence for reactivation of new faults and seismicity migration away .. The above model is the best representation of the currently active fault structures and is able to explain all the major seismological observations from 2006 to 2018 in this region. The map projection of the faults (Fig evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. 8e) show the NWF pointing in the NE direction whereas the KMF and its overlap with NWF are pointing towards the NW direction.. Active Faults in Peninsular Malaysia With Emphasis on Active Geomorphic . evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. In this paper, we summarize the results of recent geomorphic investigations of active faults in Peninsular Malaysia with emphasize on Bukit Tinggi region using IFSAR and field verification. The evidences for active faulting, and their characteristics are discussed evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Several fault segments within the Bukit Tinggi fault zone are deemed active.. National Geoscience Conference 2011 - Department Of Geology . - Yumpu evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Evidences for recent seismicities and dating of. active faulting in NW Peninsular Malaysia evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. PAPER B26. Nurul Farah Rahamat Noor, Askury Abd. Kadir & Siti Nurfarhana Mohamed. Zaid. Joint patterns of the granite in the eastern flank evidences for recent seismicities and dating of active faulting in nw peninsular malaysia

of Kledang Range, Perak evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. PAPER B27. Teh Guan Hoe & Wan Shukriyyah bt. Wan Ahamad Khalil. Occurrence of syenite and .. (a) Seismicities of Thailand (data from NEIC, TMD, and IRIS). (b .. Parts of peninsular Malaysia, and western and southwestern Thailand also exhibit evidence of active low slip rate faults or other evidence of recent tectonic movement (e.g., Fenton and Sutiwanich .. The 2015 M w 6.0 Mt. Kinabalu earthquake: an infrequent fault rupture .. Kinabalu earthquake likely resulted from the rupture of the northwest-dipping Marakau fault or a closely associated fault beneath Mt. evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. Of the faults we see in the topography, the. NATIONAL GEOSCIENCE CONFE - Yumpu evidences for recent seismicities and dating of active faulting in nw peninsular malaysia. National Geoscience Conference 2011 - Department Of Geology .. The 2015 M w 6.0 Mt. Kinabalu earthquake: an infrequent fault rupture .. More from Geoscience Letters. A short history of Japanese historical seismology: past and the present A short history of Japanese historical seismology: past and the present. Historical earthquake research in Austria Historical earthquake research in Austria. Auroral streamer and its role in driving wave-like pre-onset aurora Auroral streamer and its role in driving wave-like pre-onset aurora evidences for recent seismicities and dating of active faulting in nw peninsular malaysia.