Arc related dioritic–granodioritic magmatism from southeastern Peninsular Malaysia and its tectonic implication by Hazad, Fatin Izzani, Ghani, Azman Abd, Lo, Ching Hua

Absolute age evidence of Early to Middle Ordovician volcanism in Peninsular Malaysia by Quek, Long Xiang, Ghani, Azman Abd, Lai, Yu Ming, Lee, Hao Yang, Saidin, Mokhtar, Roselee, Muhammad Hatta, Badruldin, Muhammad Hafifi, Hassan, Meor Hakif Amir, Abdul Aziz, Jasmi Hafiz, Ng, Tham Fatt, Ali, Muhammad Afiq Muhammad, Zulkifley, Mohamad Tarmizi Mohamad

“…With these findings, the Early Palaeozoic tectonic history of Peninsular Malaysia needs careful review.…”

Seismogenic sources in the bay of bengal vis-a-vis potential for tsunami generation and its impact in the northern Bay of Bengal coast by Khan, A.A.

“…Geodynamic status, seismo-tectonic environment, and geophysical signatures of the Bay of Bengal do not support the occurrence of seismogenic tsunami. …”
Get full text

Genesis of the Selinsing gold deposit, Peninsular Malaysia: Constraints from mineralogy, geochemistry and in situ sulfur isotope compositions of sulfides by Sun, Chao, Yang, Xiaoyong, Du, Gaofeng, Abdul Aziz, Jasmi Hafiz

“…Furthermore, gold mineralization is closely related to tectonic deformation. Four main stages of vein formation have been identified, namely, (1) quartz-pyrite-arsenopyrite vein, (2) quartz-pyrite-gold vein, (3) quartz-stibnite-pyrite vein, and (4) quartz-chlorite vein. …”

Characterization of Galena and Vein Paragenesis in the Penjom Gold Mine, Malaysia: Trace Elements, Lead Isotope Study and Relationship to Gold Mineralization Episodes by Zakaria, E., Fatt, N.T., Abdul Aziz, J.H., Sebastien, M., Charles, M.

“…Trace element and lead isotope analysis was undertaken on nine samples that represent two stages of galena formed during two tectonic events. Both the Pb isotopes and the trace elements show that the first stage galena within the mineralized areas at the footwall has different geochemical characteristics compared with galena in non mineralized areas in the hanging wall, suggesting that galena crystallized from two different ore fluids and probably at two different times. …”

Study of late-Mesozoic magmatic rocks and their related copper-gold-polymetallic deposits in the Guichi ore-cluster district, Lower Yangtze River Metallogenic Belt, East China by Gu, Huangling, Yang, Xiaoyong, Nie, Zhangxing, Deng, Jianghong, Duan, Liuan, Hu, Qing, Abdul Shakoor, Mastoi, Gao, Ergen, Abdul Aziz, Jasmi Hafiz

“…Guichi region results from two episodes of magmatism probably related to tectonic transition from subduction of Palaeo-Pacific Plate to back-arc extensional setting between 150 and 125 Ma, which lead to the Mesozoic large-scale polymetallic mineralization events in southeast China.…”