week 1 - introduction.pdf

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H. Muhammad Ridha Adhari, S.T., M.Sc Dept. of Geological Engineering Faculty of Engineering Syiah Kuala University Darussalam, Banda Aceh 2016

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

Dept. of Geological EngineeringFaculty of EngineeringSyiah Kuala University

Darussalam, Banda Aceh2016

JADWAL KULIAHGeologi Dinamik, Teknik Geologi.Kuliah hari Senin, Jam 8.00-10.30 di Ruang Kuliah

Teknik Geologi.Pindah ke hari Kamis, Jam 14.00-16.30di A12-302

Tidak ada Praktikum maupun Kuliah Lapangan.

Adhari, M.R., Teknik Geologi Unsyiah

ASSESSMENTSTugas/Quiz = 20%Absensi = 10%Mid Test = 35%Final Test = 35%

Adhari, M.R., Teknik Geologi Unsyiah

SETUJU?

BOBOT NILAI AKHIR

A ≥ 8575 ≤ B+ < 8565 ≤ B < 7555 ≤ C+ < 6545 ≤ C < 5535 ≤ D < 45E < 35

Adhari, M.R., Teknik Geologi Unsyiah

RULES

Dilarang memakai sandal,celana pendek, kaos oblong.

Dilarang makan di ruangkelas, tetapi boleh minum.

Dilarang membuat keributan/kegaduhan selama kuliahberlangsung. Hargailahmereka yang serius inginbelajar.

Ketua Kelas?

COURSE OUTLINEWeek 1 : IntroductionWeek 2 : History of The UniverseWeek 3 : Interior of The EarthWeek 4 : Plate TectonicWeek 5 : QuizWeek 6 : Divergent BoundaryWeek 7 : Convergent BoundaryWeek 8 : Convergent BoundaryWeek 9 : Mid TestWeek 10 : Transform BoundaryWeek 11 : Driving MechanismWeek 12 : Hotspot and TomographyWeek 13 : Crust Deformation, Geological Hazard, Earth ResourcesWeek 14 : Final Test

Adhari, M.R., Teknik Geologi Unsyiah

REFERENCES

Adhari, M.R., Teknik Geologi Unsyiah

What is Geodynamic? The study of the physical processes that underlie

tectonic deformation. Concerned with the movement in the earth’s crust

and deformation over the scales from meters tothousands of kilometers.

Examples : mountain building, the formation ofsedimentary basins, plate tectonics, volcanoes,earthquakes.

Adhari, M.R., Teknik Geologi Unsyiah

History

Nicholas Steno George Cuvier Abraham Werner James Hutton

Charles Lyell William Smith Alfred Wegener Harry Hess

James Hall, J.D. Dana GeosynclineLeonardo da Vinci fossils were the remains ofancient life.James Ussher estimate the age of the EarthNicholas Steno Steno’s PrincipleGeorges Cuvier CatastropismAbraham Gottlob Werner NeptunismJames Hutton, Charles Lyell UniformitarianismWilliam Smith Faunal SuccessionAlfred Wegener Continental DriftHarry Hess Sea Floor Spreading

History

What Do You Think?

Adhari, M.R., Teknik Geologi Unsyiah

Adhari, M.R., Teknik Geologi Unsyiah

Adhari, M.R., Teknik Geologi Unsyiah

Rotation and Revolution

Global tomographic model of Zhao (2004)

What do you see?

What do you see?

Adhari, M.R., Teknik Geologi UnsyiahWhat Do You See?

Adhari, M.R., Teknik Geologi Unsyiah

Adhari, M.R., Teknik Geologi Unsyiah

Hotspot

Adhari, M.R., Teknik Geologi Unsyiah

Adhari, M.R., Teknik Geologi UnsyiahOcean Floor

Adhari, M.R., Teknik Geologi Unsyiah

Great Barrier Reef

Adhari, M.R., Teknik Geologi Unsyiah

Earthquake

The January 1995 Kobe earthquake destroyed this portion of the Kobe-OsakaHighway in western Japan and killed nearly 5000 people. (Atsushi Tsukada/AP WideWorld)

Adhari, M.R., Teknik Geologi UnsyiahRock Deformation

Adhari, M.R., Teknik Geologi Unsyiah

Adhari, M.R., Teknik Geologi Unsyiah

Adhari, M.R., Teknik Geologi Unsyiah

Four different types of oil traps.

Geothermal

Volcanic Eruption