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Sedimentology of the Permian Monodiexodina-bearing bed of the uppermost Kubang Pasu Formation, northwest Peninsular Malaysia: Interpretation as storm-generated, transgressive lag deposits

机译：西北半岛马来西亚的最高夸康帕苏山床沉积学，西北半岛马来西亚：解释为风暴生成，过灾滞矿床

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Meor Hakif Amir Hassan; Nur Nadwa Syahirah Al Zamruddin; Boon Sim Yeow; Ahmad Sheeqal Shah Abdul Samad;
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1. Fault analysis to Determine Deformation History of Kubang Pasu Formation at South of UniMAP Stadium Hill, Ulu Pauh, Perlis, Malaysia [J] . Adi Suryadi Journal of Geoscience, Engineering, Environment and Technology . 2016,第1期

机译：断层分析，以确定马来西亚玻璃市Ulu Pauh的UniMAP Stadium Hill南部的Kubang Pasu组的变形历史
2. Microthermometric evidence for the formation of Permian VHMS deposits in Tasik Chini area, Central Belt of Peninsular Malaysia [J] . Basori Mohd Basril Iswadi, Zaw Khin, Mernagh Terrence Patrick, Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration . 2019,第期

机译：在半岛马来西亚中央腰带中，MINIAN VHMS沉积物形成微疗证据
3. Soft-sediment deformation structures interpreted as seismites in the uppermost Aptian to lowermost Albian transgressive deposits of the Chihuahua basin (Mexico) [J] . International Journal of Earth Sciences . 1998,第4期

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4. Comparative characterization of the quaternary deposits of Northwest Peninsular Malaysia by wash boring and CPTU site investigation methods [C] . Mohamad R. Selamat, Ros N. Rosli, Muhd H. Ramli, International Conference of Global Network for Innovative Technology and AWAM International Conference in Civil Engineering . 2017

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5. Stratigraphy and sedimentology of a late Pliocene intertidal to fluvial transgressive deposit: Bacons Castle Formation, Upper York -James Peninsula, Virginia. [D] . Ramsey, Kelvin Wheeler. 1988

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6. Sedimentology of the Passage beds between the Kubang Pasu Formation and Chuping Formation, Berseri, Perlis [O] . Noorhashima Adenan, Che Aziz Ali, Kamal Roslan Mohamed 2013

机译：Kubang Pasu形成与Chuping Clowation之间穿过床的沉积学，辐射，Pllis

Sedimentology of the Permian Monodiexodina-bearing bed of the uppermost Kubang Pasu Formation, northwest Peninsular Malaysia: Interpretation as storm-generated, transgressive lag deposits

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