H. Muhammad Ridha Adhari, S.T., MJADWAL KULIAH Geologi Struktur. Kuliah hari Selasa, Jam 14.00-15.30 Ada Praktikum dan Kuliah Lapangan. Adhari, M.R., Teknik Geologi Unsyiah

H. Muhammad Ridha Adhari, S.T., M.Sc

Dept. of Mining Engineering

Faculty of Engineering

Syiah Kuala University

Darussalam, Banda Aceh

2017

JADWAL KULIAH

Geologi Struktur.

Kuliah hari Selasa, Jam 14.00-15.30

Ada Praktikum dan Kuliah Lapangan.

Adhari, M.R., Teknik Geologi Unsyiah

ASSESSMENTS

Tugas/Quiz = 10%

Praktikum = 30%

Mid Test = 30%

Final Test = 30%


SETUJU?

Praktikum

Akan dimulai pada pertemuan kelima.

Praktikum direncanakan sebanyak 10 pertemuan

termasuk UTS dan UAS.

Jadwal praktikum disesuaikan dengan jadwal asisten

dan mahasiswa.

Setiap mahasiswa akan dibagi kedalam kelompok

beranggotakan 10-15 orang.

BOBOT NILAI AKHIR


A ≥ 87

78 ≤ AB < 87

69 ≤ B < 78

60 ≤ BC < 69

51 ≤ C < 60

41 ≤ D < 51

E < 41

RULES

Dilarang memakai sandal,

celana pendek, kaos oblong.

Dilarang makan di ruang

kelas, tetapi boleh minum.

Dilarang membuat

keributan/kegaduhan.

Kehadiran minimal 75%

sebagai syarat ikut UAS.

Ketua Kelas?

COURSE OUTLINE Week 1 : Introduction

Week 2 : Primary Geologic Structure

Week 3 : Primary Geologic Structure

Week 4 : Secondary Geologic Structure

Week 5 : Quiz

Week 6 : Displacement and Strain

Week 7 : Force, Stress, Strain

Week 8 : Deformation Mechanism and Microstructures

Week 9 : Mid Test

Week 10 : Joints, Foliation and Lineation

Week 11 : Fold-Fault Interaction, Unconformity

Week 12 : Progressive Deformation & Active Tectonic

Week 13 : Final Test

Week 14 : Kuliah Lapangan




REFERENCES


Our goals

Learning how to describe the structures of rocks and

regions.

To understand the movements that accompanied

development of the structures.

To interpret structures and systems of structures in

relation to mechanics, tectonics, and geologic history.

What is geologic structure?

Geologic structure is a geometric feature in rock whose

shape, form, and distribution can be described.

Geologic Structure:

Primary Structure. Acquired in the genesis of a rock

mass.

Dike, Graded Bedding, Foliation, etc.

Secondary Structure. Result from later deformation of

the primary structures.

Faults, Fold, Joint, etc.


Geologic Structure

Primary Structure

Secondary Structure


Plate Tectonic


http://fr.cdn.v5.futura-sciences.com/sources/images/actu/rte/cyclewilson.jpgAdhari, M.R., Teknik Geologi Unsyiah

Structural Analysis

Descriptive Analysis

Kinematic analysis

Strain analysis

Dynamic analysis

Mechanism analysis

Tectonic analysis

Structural Analysis

1. Descriptive analysis

Recognizing and describing structures and measuring

their locations, geometries, and orientations.

2. Kinematic analysis

The movement paths that rocks or parts of rocks have

taken during transformation from the undeformed to the

deformed state.

3. Strain analysis

The development of mathematical tools for quantifying

the strain in a rock. Distortion (changes in shape) and

Dilation (change in size).


4. Dynamic analysis

The development of stress and its relation to deformation

5. Mechanism analysis

The study of processes on the atomic scale to grain scale

that allow structures to develop.

6. Tectonic analysis

The study of the relationship between structures and

global tectonic processes.


Descriptive analysis

Strain analysis

Dynamic analysis

For the results of a structural analysis to be

interpretable, the scale of our analysis must be taken

into account.

For example, a bed of sandstone in a single outcrop in a

mountain may appear to be undeformed. But the outcrop

may display only a small part of a huge fold that cannot

be seen unless you map at the scale of the whole

mountain.

Scale of observation :

Microscale : features that are visible optically at the scale

of thin sections (electron microscope).

Mesoscale : features that are visible in a rock outcrop, but

cannot necessarily be traced from outcrop to outcrop.

Macroscale : features that can be traced over a region

encompassing several outcrops to whole mountain ranges.

Megascale : continental-scale deformational, such as the

movements of tectonic plates over time.


Each scale of observation has its own set of tools :

Microscale : Optical and electron microscopes are

used.

Mesoscale : recognition and description of rocks

requires a set of eyes, a hammer, a compass, and a

hand lens.

Macroscale, Megascale : Satellite imaging may be

used for observations.


microscale

mesoscale

mesoscale

macroscale

macroscale

What Do You See?

macroscale

What Do You See?

Ulee lheu, Aceh Besar

What Do You See?

Ujong Pancu, Aceh Besar

What Do You See?

Lhong, Aceh Besar

What Do You See?

Lhong, Aceh Besar

What Do You See?

Indrapuri, Aceh Besar

What Do You See?

Lhong, Aceh Besar

What Do You See?

Petroleum exploration

Ore deposits geology

Geothermal System

Hydrogeology

Building Construction

Geological Hazard

Uses of Structural Geology

Petroleum System

Petroleum System

Common oil traps


Ore Deposits

Ore Deposits

Hydrogeology

Geothermal

Tsunami

H. Muhammad Ridha Adhari, S.T., MJADWAL KULIAH Geologi Struktur. Kuliah hari Selasa, Jam 14.00-15.30 Ada Praktikum dan Kuliah Lapangan. Adhari, M.R., Teknik Geologi Unsyiah

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