GEOLOGI UKM Paling Gempak!: 2013

Tuesday, 10 December 2013

PEMBENTANGAN LATIHAN ILMIAH I
(SESI 2013/2014)

Penyelaras memberi ucapan

Pembentangan oleh Farhan & Aliff

Dr. MRU mempengerusikan Majlis Penutup

GeoLadies

GeoBro

Hakiem : Pembentang Terbaik

Ain Alya : Pembentang Terbaik

SESI BERGAMBAR BERSAMA PENSYARAH GEOLOGI

6 PEMBENTANG TERBAIK LATIHAN ILMIAH I

"TAHNIAH! kepada semua pelajar Geologi Tahun 3 UKM kerana telah berjaya membentangkan hasil kajian tesis masing-masing dalam siri Seminar Latihan Ilmiah 1, Sesi 2013/2014. Jadikan latihan pembentangan kali ini sebagai pengalaman yang berguna untuk membina kerjaya anda sebagai ahli geologi yang berjaya." - Dr. Wan zuhairi Wan Yaacob

Friday, 29 November 2013

GEOSKILLS III : CARA BELAJAR DALAM GEOLOGI

KULIAH :

Pembelajaran secara langsung/terus daripada pensyarah kepada pelajar *memberi kefahaman terhadap fakta, teori dan memberi pengetahuan lebih daripada bahan pembelajaran & bacaan. *appreciate apa yang dipelajari

Prof. IBA memberi penerangan

Amali :

Pembelajaran secara 'hands on' dan praktikal *faham, mengaplikasikan kaedah, penerangan semula dan kenalpasti cirian utama

LAPANGAN :

Pengajaran secara terbuka (critical thinking) : mengaplikasikan pengetahuan teori, amali dan pengetahuan umum geologi, analisis dan interpretasi

KUIz DAN PEPERIKSAAN

Ujian kefahaman, pengolahan fakta dan menguji tahap pengetahuan

PERBINCANGAN DAN PERKONGSIAN

Pembelajaran berdasarkan kefahaman orang lain untuk mendapat penjelasan & membuat penambahbaikan serta menguji ketepatan

BACAAN, RUJUKAN & PENIRUAN

Pembelajaran secara sendiri untuk memupuk kefahaman dengan lebih lagi

Sumber : Bilik Sumber Geologi

PENGALAMAN :

Pengalaman orang lain seperti Mentor, tutor, alumni, senior untuk mendapat gambaran dan pengalaman sebenar. Kesempatan untuk maju kehadapan

Perkongsian Alumni

PENGLIBATAN AKTIVITI/PROGRAM :

Pembelajaran secara tidak langsung dan pendekatan memperolehi ilmu dengan lebih menarik contohnya menyertai 'Conference' Geologi

Oil & Gas Festival UTM Skudai

"Work the system by Understand the system"

Sunday, 10 November 2013

LECTURE, LAB & FIELDWORK
#2nd year #Geology #Petrology #Sedimentology #Structural Geology #Mapping Techniques
(Laugh, Osem, Life = LOL )

#T. Pemetaan : 1st time, analsis Peta Topo & Peta Geologi

#Petrologi...macam comel je..macam cantik je haha

kita belajar "Sedimen".. apa dia??.. "Sedimen" XD

#Sedimentologi :Sesi belajar dan bersembang (mengenai Geologi jugak ) :P

"#Geologi struktur mengkaji struktur-struktur geologi"

#Fieldwork
Rutin setiap sabtu & ahad

Taman Pantun UKM

Sungai Tekala

Port Dickson

Ayer Hitam, Johor

Geologi Struktur, Temerloh, Pahang

#Mapping #Laporan

Gandingan terbaik : Farhana & Raymond

En. Amirul Interframe

Fatiha & Azura

_______________________________________________________________________________

Introducing our batch Jersey <3

Oil & Gas Festival UTM Skudai

"Our differences they do a lot to teach us how to use the tools and gifts we got, yeah we got a lot at stake" =)

ROLE OF GEOSCIENCE IN OIL & GAS INDUSTRY

Baker Hughes Tecnical Talk : Univ. Malaya

Date : NOV 13th, 2013 (Wednesday)

SPEAKER I : WONG KUM SENG

Technical Manager, Drilling and Evaluation at Baker Hughes

SPEAKER II : MIKE ORR
Geoscience Advisor at Baker Hughes

It is such an honor to us, the undergraduates of Geology UKM to be a part of Baker Hughes Technical Talk organized by UM AAPG SC and we would like to express our highest gratitude to the organizer for having us in this program.

The objective of this event is to give the Geology students a basic insight to the world of oil & gas industry and to explain in details the role of geosciences in this industry.

In general, the presenters had started with the introduction to O&G industry and exposed us to the technology used in geosciences exploration, fundamental aspect in evaluation and ended it with a sharing session of their experiences within 2 decade of involving in this industry.

“It was an eye opener event, it has really explained the working atmosphere in the industry. Congratulations to both of the presenters for such an amazing effort, million thanks to all of geology UM's students for the warm welcome and we truly enjoyed it so much"

Students of Geology UKM & Geology UM

Friday, 8 November 2013

KETIKA GEOLOGIST BERSAJAK [Nukilan: Siswandi Kastari]

Bila Anortit kau anggap dosa..
Maka jadilah Granit..
Namun usaha dan doa mu untuk Pegmatit
Karena bila tidak..bukan hanya kau akan mem-Basalt Gabro
Tapi bisa jadi Peridotit Dunit Kau...

Lalu kenapa berdiam dalam Diorit Andesit?..
Kiri tidak Kanan pun bukan..
Buang semua Andesin Bitownit dalam diri..
Ingat!.. sehalus apapun Albit..
Paling tidak kau akan sampai pada Ryolit..
Dan Ryolit itu dekat kepada Granit...

Jadi perbanyaklah Albit..
Sering-seringlah berQuarsa..
Dan.. lakukan itu semua dengan Orthoklas..
Dan bila kesabaran ada padamu..
Granit pun terlampaui.. Pegmatit kau nanti..

Makna-makna perumpamaan mineral dalam sajak ini (translate)
1. mineral2 mafik bewarna gelap menunjukkan sifat2 buruk (keburukan)
2. mineral2 felsik berwarna cerah menunjukkan sifat2 mulia (kebaikan)
3. batuan mafik menunjukkan org yang berakhlak buruk, ultramafik : org yg sgt x baik
4. batuan felsik (Granite) menunjukkan org yang berakhlak baik, pegmatite : org yg sgt baik

Friday, 1 November 2013

ROOT CAUSES OF EXTENSIVE MASS MOVEMENTS IN KUNDASANG SABAH

H.D Tjia

Universiti Kebangsaan Malaysia

Root cause 1 : two active regional fault - Mensaban & crocker zones. Trusmadi Formation in the study area consists of old submarine slump deposits associated with Kinabalu Suture. zones within the formation are phyllonitic with the competent clasts deformed as sigmoids, all clearly resulting from shearing

Root cause 2 : The mass movement of Kundasang involve these chaotic deposits that generated ground movements upon exposure and most probably drainage disturbance through accelerated landuse.

Root cause 3 : The Kinabalu felsic pluton became emplaced in a span of 9 to 4 million years. Plutonic intrusion can be estimated to have occured at 4km or deeper depth. Now the top of pluton reaches 4095m above sea level. This implies that average annual uplift of the pluton has ranged between 0.9 to 2.03mm. It may be safely assume that the Kinabalu intrusive body is still rising as the summit plateau of glacially sculpted surface is disturbed by normal faults with downthrows of more than 10m.