2 type-movement-boundary of plates
DESCRIPTION
geologiTRANSCRIPT
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Modul 2
-Type of lithosphere (type of plate)
-Movement of plates
-Type of plate boundaries
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BUMI DALAM PERSPEKTIF RUANG ANGKASA
* ATMOSFER & HIDROSFER
* BIOSFER
* KONTINEN & SAMUDERA
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GAMBARAN PERMUKAAN BUMI
MEMBERIKAN REKAMAN DARI DINAMIKA BUMI
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GAMBARAN UTAMA
PERMUKAAN BUMI
KONTINEN
Shield, Stable platform,
Folded mountain
SAMUDERA
Oceanic Ridge, Abyssal,
Seamounts, Trench,
Continental Margin
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Evidence on Seafloor
Seafloor Age Map
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Deformation history of the Eastern Belt,
Peninsular Malaysia
Ibrahim Abdullah
Program Geologi, Fakulti Sains dan Teknologi
Universiti Kebangsaan Malaysia
Bangi, 43600, Selangor DE.
Malaysia
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Tree Belts:Western,Central,
Eastern
Originally proposed by
Scrivenor (1928)
Western boundary:
- Connecting serpentinite bodies
- Known as Bentung Line,
Hutchison ((1975)
- Could extend southwards,
> Across straits of Malacca
> Through Lalang Fault Zone
> Known as Bentung Suture
(Tjia, 1987)
Eastern boundary-Lebir Fault zone
TE CTO N IC B E LTS
O F MALAYS IA PE N IN S U LA
EA
STE
RN
BELT
CEN
TRA
L BELT
WESTE
RN
BELT
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2. General Geology of the Eastern Belt
= Oldes sediment-Carboniferous and Permian
> Clastic, volcanic and minor lst.
> Plant fossils ( Chand, 1978; Jennings, 1985)
> Fauna (trilobites, brachiopod, bryozoans, bivalves
(Idris and Zaki, 1986)
Plant
fossils
Clastic
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- Linear belt of Triassic-Jurassic (Chung1973)
- Late Permian-tuffaceous sst., slst. And
mst.+cgl. (Tiemoko et.al, 1992)
- Jurassic-Cretaceous continental deposits-
Gagau group (Rishworth, 1974)
Pulau
Redang
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STRUKTUR BUMI : C-M-C(compositionally)
Inti Bumi (Core)
Selubung (Mantle)
Kerak (Crust)
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STRUKTUR BUMI
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STRUKTUR INTERNAL BUMI
PENJALARAN GELOMBANG SEISMIK DIDALAM BUMI
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STRUKTUR BUMI
PERUBAHAN KECEPATAN GEL. P & S PADA KEDALAMAN
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LITHOSFER & ASTENOSFER(mechanical properties)
LITHOSFER
Lapisan terluar (100 km) kuat,
kaku (rigid), terdiri dari kerak
bumi & sebagian mantel atas
ASTENOSFER
Lapisan lunak pada mantel
atas (100-200 km), dibawah
litosfer, dekat titik lebur batuan
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De
pth
(k
m)
cold, rigid, brittle
hot, plastic
hot, high pressure,rigid, brittle
liquid
solid
rocks
ultrabasicigneous rocks
Fe, Ni
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Kerak bumi merupakan lapisan paling luar: keras,
padat, relatif dingin, ketebalan 70 - 100 km,
tersusun dari batuan beku, batuan sedimen, dan
batuan ubahan.
Kerak bumi dibedakan menjadi dua:
Kerak Samudra danKerak Benua
KERAK BUMI
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STRUKTUR BUMI
LITHOSFER & ASTENOSFER - KERAK & MANTEL
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GAMBARAN PERMUKAAN BUMI
RANGKAIAN PEGUNUNGAN
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JALUR STRUKTUR UTAMA
GAMBARAN PERMUKAAN BUMI
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STRUKTUR BUMI
DISTRIBUSI PUSAT GEMPA
GAMBARAN PERMUKAAN BUMI
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STRUKTUR BUMI
RANGKAIAN GUNUNG API
GAMBARAN PERMUKAAN BUMI
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KONFIGURASI (MOSAIK) LEMPENG
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Plate Tectonics
What drivesPlate Tectonics???
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GEODYNAMICS
TektonikLempeng 36
GERAK LEMPENG
DAYA PENGGERAK (Driving Forces)
- Slab Pull
- Push Ridge
- Basal (mantle) Drag
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What drives plate motions Forces that drive plate motion
Slab-pull
Cold, dense slabs of subducted oceanic lithosphere pull the plate towards the subduction zone
Ridge-push
The higher elevation of spreading centers result in oceanic lithosphere wanting to move downhill, away from the ridge
Far less important than slab-pull
Mantle drag and plate resistance
Can act to increase or decrease plate motion
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GEODYNAMICS
TektonikLempeng 38
DAYA PENGGERAK
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GEODYNAMICS
TektonikLempeng 39
DAYA PENGGERAK
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GEODYNAMICS
TektonikLempeng 40
DAYA PENGGERAK
PUSH RIDGE
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Internal Heat
Plate Tectonics
Basal / Mantle drag
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GEODYNAMICS
TektonikLempeng 42
3 KEMUNGKINAN KONVEKSI PADA MANTEL
3 KEMUNGKINAN KONVEKSI
MANTEL
- Pada Astenosfer
- Pada keseluruhan Mantel
- Timbul dari Batas Inti-Mantel
(Mantel Plume)
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Models of plate-mantle convection Any model must be consistent with
observed physical and chemical properties of the mantle
Horizontal movement of plates causes mantle upwelling
Models Layering at 660 km Explains why basalts erupted at
mid-ocean ridges are different (more evolved, relatively shallow source) compared to those erupted at hot-spots (more primitive, deeper source).
We know that subducting slabs descend beneath 660 km
What drives plate motions
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Model of Whole-mantle convection
Would mix the entire mantle in the space of a few hundred million years, removing heterogeneities
What drives plate motions
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Deep-layer model
Lava lamp model
Two layers swell and shrink in a complex fashion in response to heat from the Earths interior
What drives plate motions
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GEODYNAMICS
TektonikLempeng 46
KECEPATAN GERAK LEMPENG
GERAK RELATIF LEMPENG
- Paleomagnetisme
- Studi Mekanisme Fokus Gempa
GERAK ABSOLUT LEMPENG
- Hot Spot
- GPS
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GEODYNAMICS
(Kearey et al 2009)
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GEODYNAMICS
TektonikLempeng 48
KECEPATAN GERAK LEMPENG
PENENTUAN UMUR DAN PERTUMBUHAN
SAMUDERA DARI PALEOMAGNETISME
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Evidence on Seafloor
PENENTUAN UMUR DAN PERTUMBUHAN SAMUDERA DARI PALEOMAGNETISME
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Evidence on Seafloor
Seafloor Age Map
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GEODYNAMICS
TektonikLempeng 51
KECEPATAN GERAK LEMPENG (relatif)
PENENTUAN KECEPATAN DARI GERAK LEMPENG (FOKUS GEMPA & GPS)
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GEODYNAMICS
(Kearey et al 2009)
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Mantle Plume Hot Spot Tracks
Evidence on Seafloor
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(Kearey et al 2009)
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GEODYNAMICS
TektonikLempeng 55
KECEPATAN GERAK LEMPENG (absolut)
PENENTUAN KECEPATAN GERAK LEMPENG DARI SEAMOUNTS (ABSOLUT)
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HOTSPOTS
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GEODYNAMICS
TektonikLempeng 59
KECEPATAN GERAK LEMPENG
KECEPATAN GERAK LEMPENG DAN PERTUMBUHAN SAMUDERA
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Directions of Motion and Plate Velocities Determined by
Mantle Plume Hot Spot Tracks and Age-Dating of Rocks
Plate Tectonics
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Directions of Motion and Plate Velocities Determined by GPS
(Global Positioning System) Satellites
Plate Tectonics
Directions of Motion and Plate Velocities Determined
by GPS (Global Positioning System) Satellites
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(Kearey et al 2009)
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(Kearey et al 2009)
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Plate boundaries
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BASIC PLATE TECTONICS Revised
Earths lithosphere is broken into 12-24 rigid
plates
Plates move about 1-10 cm/yr on the plastic
Asthenosphere
Geology happens where the plates
interact with one another along Divergent,
Transform, Subduction and Collisional
Boundaries
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Results in the formation of Oceanic Crust
Plate Tectonics
Divergent Boundary
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Transform Boundary
Plate Tectonics
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Results in the formation & growth of Continental Crust
and destruction of Oceanic Crust
Melting
Produces
More
Felsic
Magma
Plate Tectonics
Convergent Boundary: Subduction
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Results in the growth of Continental Crust
Convergent Boundary: Collision
Plate Tectonics
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TEKTONIK LEMPENG (PLATE TECTONICS)
BATAS DIVERGEN, KONVERGEN & STRIKE-SLIP
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GERAK DIVERGEN, KONVERGEN & STRIKE-SLIP
TEKTONIK LEMPENG
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TEKTONIK LEMPENG
CONTINENTAL MARGIN SREADING CENTER
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TEKTONIK LEMPENG
SPREADING CENTER (PUSAT PEMEKARAN)
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TEKTONIK LEMPENG
PERTUMBUHAN SAMUDERA
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TEKTONIK LEMPENG
CONVERGENT, CONTINENT-OCEAN,
OCEAN-OCEAN, CONTINENT-CONTINENT
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TEKTONIK LEMPENG
SUBDUCTION &VOLCANISM
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TEKTONIK LEMPENG
SUBDUCTION & EARTHQUAKE
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TEKTONIK LEMPENG : polyhistory
COLLISION & STRIKE-SLIP
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INTRAPLATE VOLCANISM
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GEODYNAMICS
TERIMAKASIH
TektonikLempeng 83