kuliah geologi dasar kelas a 2014-2015 1&2

8/19/2019 Kuliah Geologi Dasar Kelas a 2014-2015 1&2

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OUTLINE MATERI PERKULIAHAN MK GEOLOGI DASAR2014

1. PLANETARIUM, sebagaiperba!iga "P#ae$ar%&Ear$'()*paris)+

2. ISIS-GEOISIKA UMI "PH/SI(ALEARTH+ I$eri)r *i Kera *i

3. PERMUKAAN UMI, e$agA#a*-Ge)*)r)#)gi

4. ENOMENA ALAM "Ge)#)giDia*is+

1. K)sep Te$)i Le*peg

2. Se!i*e$asi3. Mag*a$is*a-5)#ais*a

4. Pe$ari'a U*r *i

6. SUMERDA/A GEOLOGI

1.Miera#, a'a

Ga#ia,2. Hi!r)arb)-Migas,

a$bara

3.Paas *i4.S*ber!a%a Air

7. POTENSI EN(ANA Isse *i

Pa!a Masa Kii "Re8e$+1.Ge*pa *i,

L)gs)r, a9ir,Le$sa Gg Api, Tsa*i, Se*braL*pr

2.Pe*aasaG#)ba#-Ee R*a'Ka8a, G#asiasi


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Kuliah SUB POKOK BAHASAN ARAHAN MATERI

1 Pendahuluan Pengertian Pengenalan Ruang Lingkup

25-Agustus-14 Tinjauan Umum Pembahasan mata kuliah

Tujuan Mata Kuliah Pengantar lmu !e"l"gi

2 Prinsip lmu !e"l"gi #istem lmu Kebumian Kepentingan$aplikasi lmu !e"l"gi

%1-#ep-14 Landasan Pemikiran lmu ge"l"gi K"nsep studi dan sejarah ge"l"gi

&ukum-hukum dasar !e"l"gi 'Tekt"nik Lempeng( #iklus!e"l"gi)

Uni*"rmitarisma and Katatr"*isma

4 Kajian lmu !e"l"gi %+-#ep-14 Ph,sial !e"l"g, dan &,st"rial !e"l"g, .abang dan pembahasan keilmuan !e"l"gi

5 #kala /aktu !e"l"gi Met"da Pentarikhan ge"l"gi 0eterminasi /aktu !e"l"gi

Rek"nstruksi #kala /aktu !e"l"gi Pentarikhan Relati* dan abs"lut

#kala #pasial !e"l"gi 15 #ep-14 Rek"nstruksi Pr"ses !e"l"gi #kala Mikr"sk"pis - .ekungan

Material 3umi 22-#ep-14 Materi Pen,usun 3umiPengenalan dan deskripsi mineral dan batuanPr"ses pembentukan batuan

Mineral dan 3atuan '#edimen( Metam"r*(3eku) Lingkungan pembentukan batuan

+

Ujian Tengah #emester Ujian Lisan

1% 0inamika !e"l"gi 0e*"rmasi batuan dan metam"r*isma Analisis m"del sederhana bentuk hasil de*"rmasi batuan

%-t-14 6ulkanisma Kegiatan ekstrusi dan erupsi( pembentukan dan pr"duk gunungapi

Tekt"nik Lempeng Pengertian( jenis dan gerakan lempeng

Pemekaran Lantai #amudera Pengertian( jenis dan pemekaran lantai samudera

K"ntinental Margin Pengertian( jenis dan k"ntinental margin

11 Kebenanaan !e"l"gi7en"mena kebenanaan dan ge"l"gilingkungan Pemahaman jenis dan intensitas kebenanaan

18-t-14 !empa 3umi 7akt"r pen,ebab dan pen,ebaran kebenanaan

!erakan Tanah dan 3anjir Pemahaman k"ndisi !e"l"gi Lingkungan

12 #umberda,a Air 18 t 14 9enis dan klasi*ikasi sumberda,a air :lemen dasar keterdapatan sumberda,a air

#umberda,a Mineral 2% t 14 9enis dan klasi*ikasi sumberda,a mineral :lemen dasar keterdapatan sumberda,a mineral

18#umberda,a :nergi dan!e"thermal 2% t 14 9enis dan klasi*ikasi sumberda,a energi :lemen dasar keterdapatan sumberda,a energi

14 Kuliah Lapangan24-2 t 14

Pengamatan lapangan15 Presentasi Kel"mp"k 2 t 14

1 Ujian Akhir Desember 2014 Ujian Lisan

SATUAN ACARA PERKULIAHAN MATA KULIAH GEOLOGI DASAR

SEMESTER GENAP 2014/2015 KELAS A


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THE DIAGRAM SHO:S THE MAIN (OMPONENTS O THEEARTH;

G E O S C

I E N C E


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INTRODUCTION TO BASIC GEOLOGY

1; The


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Wh !" a #e"l"$ !e$ree%

!e"l"g, is a great Ba, t" use ,"ur sienti*i

training t" s"l=e real B"rld pr"blems;

Thr"ugh eCtensi=e *ieldB"rk( !e"l"g,

de=el"ps ,"ur Ds"*t skillsD in Ba,s that the

maj"rit, "* "ther subjets ann"t d";

!e"l"g, gi=es ,"u Bide and eCellent areer"pp"rtunities;


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!:L!#T# AR: :MPLE:0 < 06:R#:

..UPAT


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/h, d" !e"l"g,H

!e"l"g, is "nerned Bith understanding the

e="luti"n "* planet :arth and the #"lar #,stem; t deals Bith *undamentals suh as the "rigin "*

the hemial elements( the hist"r, "* li*e( and pr"esses that range *r"m atal,smi t" alm"st

impereptible;

!e"l"g, "mbines all "* the basi sienes t"ansBer @uesti"ns that a**et all "* "ur li=es "n

:arth;


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UMI SEAGAI TEMPAT KITA HIDUP, SEHINGGA PERLU KITAPAHAMI PERILAKU DAN HAITUASI DARI UMI. (ONTOHN/AMERESPON POTENSI EN(ANA SEMA(AM GEMPA UMI, GUNUNGMELETUS, LONGSOR, AN>IR, TSUNAMI, SERTA MEN>AGAKELESTARIAN UMI SEAGAI LINGKUNGAN HIDUP?.EARTH

PRO(ESS

UMI SEAGAI TEMPAT /ANG MEN/EDIAKAN KEUTUHAN DANMENOPANG TUMUH KEMANG PERADAAN MANUSIA,KHUSUSN/A ATAS KETERSEDIAAN SUMERDA/A MINERAL, AIR,AHAN GALIAN DAN ENERGI??.EARTH MATERIAL

DIPERLUKAN PEMAHAMAN /ANG ERHUUNGAN DENGAN DIMANADAN AGAIMANA KITA MENEMUKAN SUMERDA/A TERSEUTSERTA AGAIMANA MEMANAATKANN/A??EARTH HISTOR/

Hanya Satu Bumi …….


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#e"l"$is&s S&u!

Ear&h Pr"'esses


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#e"l"$is&s S&u!

Ear&h Pr"'esses


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#e"l"$is&s S&u!

Ear&h Pr"'esses


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7"t" "leh 9iji Press( T"ru Eamanaka(T"shi*umi

Kitamura$A7P$!ett, mages#el( 5 Mar 2%18


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21 June 2006

SIDOARJO MUD VOLCANO (?)

Diapirism /overpressured shale

#e"l"$is&s S&u! Ear&h Pr"'esses


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SIDOARJO MUD VOLCANO (?)20 Octoe! 2006


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06 A"!#$ 200%

SIDOARJO MUD VOLCANO (?)


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#EO(O#ISTS STUD) EARTH MATERIA(S

COAL

PETROLEUM

GOL&


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Wha& *"+&r"ls &he Dis&ribu&i"+ ",Wha& *"+&r"ls &he Dis&ribu&i"+ ",

Na&ural Res"ur'es%Na&ural Res"ur'es%IN&ONESIA OIL'GAS (ASIN


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IN&ONESIA OIL'GAS (ASIN


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IN&ONESIAN METAL


Na&ural Res"ur'es%Na&ural Res"ur'es%


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Mi+eral Res"ur'es%Mi+eral Res"ur'es%


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:ART& &#TRE

The hist"r, "* hanging en=ir"nments "n :arth;

3ased "n the re"gniti"n "* the signature "* hanging en=ir"nments

"=er time( as preser=ed in the r"k;

:


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25/76

Sea Level Changes


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A 8ar$)) ) $'e g#)ba# 8arb) 8%8#e. P))#s "i b#a8+ aregiga$)s "1G$ @ 110= T)s+ ) 8arb), a! Bes "iprp#e+ are G$ 8arb) per %ear. I##s$ra$i) 8)r$es%NASA Ear$' S8ie8e E$erprise.

CNASA


27/76

Ti*e series r)* air 8)##e8$e! appr)i*a$e#% ee#% i g#ass 8)$aiers a!re$re! $) GMD )r aa#%sis. Sares are $')g'$ $) be regi)a##%represe$a$iFe p#ses are $')g'$ $) be iBe8e! b% #)8a# s)r8es a!sis. A s*))$' 8rFe a! #)g&$er* $re! are $$e! $) $'e represe$a$iFe*easre*e$s 'e s8ie$ !a$a eis$. Da$a s') i GRA/ arepreliminary. A## )$'er !a$a 'aFe !erg)e rig)r)s a#i$% assra8e a!are ree#% aFai#ab#e r)* GMD, (DIA(, a! :MO :D(GG.

ftp://ftp.cmdl.noaa.gov/ccg/http://cdiac.esd.ornl.gov/http://gaw.kishou.go.jp/wdcgg.htmlhttp://gaw.kishou.go.jp/wdcgg.htmlhttp://cdiac.esd.ornl.gov/ftp://ftp.cmdl.noaa.gov/ccg/


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!l"bal .limate .hanges sine last e Age

What are the obvious changes observed?What are the obvious changes observed?

What might be the reasons that contribute to producing change ?What might be the reasons that contribute to producing change ?

2)*000 +e,!- A.o2)*000 +e,!- A.o To,To,


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Understanding "ur :n=ir"nment #l"bal 'ha+$e &hr"u$h &ime

#table C,gen s"t"pe re"rd G :arths limate has

=aried "nsiderabl, "=er ge"l"gial time Sea (e-el Rise

Related t" retreat "* the last "ntinental glaiers

The e Age G neB Barmer limate makes the :arth

m"re h"spitable *"r humans

Atm"spheri temperature rise n"B als" "ntributing t" additi"nal rise in sea le=el G h"B Bill this impat

"astal itiesH


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Geology is the study of the

Earth.– Physical geology is concerned with the

materials and processes which compose

and operate on the surface of, and within,Earth.

– Historical geology is concerned withthe origin and evolution of Earth's

continents, oceans, atmosphere, and life.


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:arth #truture

Wha& Is I+si!e Ear&h%Wha& Is I+si!e Ear&h%


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What Is Inside Earth?What Is Inside Earth?

continental continental oceanic oceanic

mantlemantle

#!onn#c3e$ co!e#!onn#c3e$ co!e -o$#-o$#

o$teno$ten

c!u-t

,nt$e

co!e


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Ear$' s$r8$re & T'e 8)*p)si$i)a# a! *e8'ai8a##a%ers ) $'e ear$'.


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H". D"es #e"l"$ I+,lue+'e Where We (i-e%H". D"es #e"l"$ I+,lue+'e Where We (i-e%

L,n-$#e-L,n-$#e-

o$c,n#co$c,n#c

e!u"t#on-e!u"t#on-

,u$t-,u$t-

So#$ T"eSo#$ T"eR#7e!-R#7e!-


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Wha& Pr"'esses A,,e'& Our Pla+e& I+&er+all a+! E/&er+allWha& Pr"'esses A,,e'& Our Pla+e& I+&er+all a+! E/&er+all HH

G!,7#t,t#on,$ "u$$G!,7#t,t#on,$ "u$$

Ato-"8e!#c Ato-"8e!#c

"!e--u!e"!e--u!e

ee

$$

eecc

t! t!

oo

,,

..nn

ee

t#t#

cc

G!,7#tG!,7#t

o!ce- 9#t8#n E,!t8o!ce- 9#t8#n E,!t8R,#o,ct#7e ec,R,#o,ct#7e ec,

He,tHe,t

He,tHe,t

9#n

oce,n

cu!!ent-

PEMIKIRAN )AN# MERUPAKAN (ANDASAN


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PEMIKIRAN )AN# MERUPAKAN (ANDASAN

#EO(O#I SEBA#AI I(MU

(EONARDO DA IN*I 142 3 11 5

G .angkang-angkang kerang ,ang sudah mem*"sil ditemukan di Pegunungan Apenina( talia( sebagai bekas kehidupan laut

dan bahBa talia pernah suatu ketika digenangi laut;

NI*O(AS STENO 1678 3 1689 5 G Eang memperhatikan pelapisan-pelapisan batuan menerbitkan hasil pengamatann,a bahBa batuan ,ang terbentuk labih

dahulu terletak lebih baBah dari ,ang terbentuk kemudian;

G 0engan prinsip itu maka #ten" dapat mengenal bagaimana batuan telah terlipat

Daur #e"l"$i :AMES HUTTON 198 5 *HAR(ES ()E(( 1870 5;

G Muka bumi senantiasa diremajakan "leh pr"ses tekt"nik dan pr"ses denudasi ,ang berulang-ulang;

Hu


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Priniples 7 !:L!E

Priniple "* #uperp"siti"n

Priniple "* riginal &"ri?"ntalit,

Priniple "* riginal Lateral ."ntinuit, Priniple "* ntrusi=e Relati"nships

Priniple "* .r"ss-.utting Relati"nships

Priniple "* 7"ssil #uessi"n G Billdisuss in 3i"stratigraph, #eti"n


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Priniple "* #uperp"siti"n

n an, unde*"rmed se@uene "* sedimentar,

r"ks( eah bed is ,"unger than the "ne bel"B it

and "lder than the "ne ab"=e it;

This is the basis "* relati=e ages "* all strata and

their "ntained *"ssils;


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De&ermi+i+$ &he Se=ue+'e ", Pas& $e"l"$i' E-e+&sDe&ermi+i+$ &he Se=ue+'e ", Pas& $e"l"$i' E-e+&s

Priniple "* #uperp"siti"n)

#andst"ne#andst"ne

The ,"ungest la,er is "n t"pThe ,"ungest la,er is "n t"p

Metam"rphi r"ksMetam"rphi r"ks

Or!er ", Su>er>"si&i"+Or!er ", Su>er>"si&i"+


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Priniple "* riginal &"ri?"ntalit,

#ediments usuall, *"rm *lat-l,ing dep"sits

"n the earths sur*ae;

#edimentar, r"ks are h"ri?"ntal beause

the "riginal sediments Bere h"ri?"ntal


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Principle of Original Lateral Continuity


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( , I l i( , I l i


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A oun.e! !oc3 c,n A oun.e! !oc3 c,n

#nc$ue "#ece- o; ,n#nc$ue "#ece- o; ,n

o$e! !oc3o$e! !oc3

+oun.e!+oun.e!O$e! O$e!

(a. ", I+'lusi"+s(a. ", I+'lusi"+s

Priniple "* .r"ss .utting Relati"nships


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A ge"l"gi *eature is ,"unger thanA ge"l"gi *eature is ,"unger than

an, r"k "r *eature it r"ssutsan, r"k "r *eature it r"ssuts

7aults r"ssutting7aults r"ssutting

preeCisting la,ers preeCisting la,ers

Priniple "* .r"ss-.utting Relati"nships


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Direct ContactDirect Contact

So$##;#e M,.,So$##;#e M,.,

(,3e Roc3-(,3e Roc3-

une!.!ounune!.!oun

(,3e Roc3- on(,3e Roc3- on

t8e Su!;,cet8e Su!;,ce


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Rela&i-e Da&i+$ ", R"'


48/76

Th R k C


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The Rock CyceThe Rock Cyce

E!o-#on ,n t!,n-"o!tE!o-#on ,n t!,n-"o!t=e,t8e!#n.=e,t8e!#n.

&e"o-#t#on&e"o-#t#on

&e;o!,t#on ,n et,o!"8#-&e;o!,t#on ,n et,o!"8#-

Me$t#n.Me$t#n.

So$##;#c,t#onSo$##;#c,t#on

(u!#,$ ,n $#t8#;#c,t#on

Uni!or"itarianis"


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Uni*"rmitarianism

*"+&i+ui& ", *ause a+! E,,e'&

Appl, .ause and :**et t" 7uture -

Prediti"n

Appl, .ause and :**et t" Present -

Tehn"l"g,

Appl, .ause and :**et t" Past -

Uni*"rmitarianism


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Uni*"rmitarianism d"es not meanF

.atastr"phes ne=er "ur

Ph,sial ."nditi"ns "n :arth ne=er .hange

:arth has alBa,s been the same Ph,sial pr"esses alBa,s "ur at the same rate

"r intensit,

LaBs "* Ph,sis ha=e alBa,s been the same


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Uni*"rmitarianism does meanF

Usi+$ "ur hsi'al la.s? .e 'a+

&es&;

/hether atastr"phes ha=e "urred /hether ph,sial "nditi"ns "n earth ha=e

hanged( and i* s"( h"B 'ie ages( Barm peri"ds(

high "r l"B sea le=el( et;)

/hether ph,sial laBs themsel=es ha=e hanged

in time( "r elseBhere in the uni=erse;


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Ho# can #e in!er the En$iron"entHo# can #e in!er the En$iron"ent

in #hich a rock !or"ed?in #hich a rock !or"ed?

10 C

N S


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> C


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Ho# can #e in!er the "echanis"Ho# can #e in!er the "echanis"


Ho# Do Ma%s and SateiteHo# Do Ma%s and Sateite


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Ho# Do Ma%s and SateiteHo# Do Ma%s and Sateite

I"a&es He% Us St'dy Earth(sI"a&es He% Us St'dy Earth(s

S'r!ace ?S'r!ace ?

To"o.!,"8#c ,"To"o.!,"8#c ,"

S8,eS8,e

Re$#e;Re$#e;M,"M,"

S,te$$#te #,.eS,te$$#te #,.e

Geo$o.#c ,"Geo$o.#c ,"

R ti G i ) t i thRe%resentin& Geoo&ic )eat'res in the


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Re%resentin& Geoo&ic )eat'res in theRe%resentin& Geoo&ic )eat'res in the

S'*s'r!aceS'*s'r!ace

C!o-- -ect#onC!o-- -ect#on

($oc3 #,.!,($oc3 #,.!,

St!,t#.!,"8#cSt!,t#.!,"8#c

-ect#on-ect#on

>&>&

2&2&

1&1&


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P$,te tecton#c- #- t8e un#;#n. t8eo! o; .eo$o.

P$,te tecton#c- #- u-e;u$ #n t8e ;#e$ o; .eo$o. ec,u-e #t c,n e

u-e to e?"$,#n , 7,!#et o; .eo$o.#c "!oce--e-* #nc$u#n.

7o$c,n#c ,ct#7#t* e,!t8@u,3e-* ,n ount,#n u#$#n.

Plates and Boundaries (Side View)

http://encarta.msn.com/encnet/refpages/RefArticle.aspx?refid=761554623http://encarta.msn.com/encnet/refpages/RefArticle.aspx?refid=761554623


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61

McKnight and Hess. 2002. Physical Geography.

Interna )orces Tectonis" +ocanis"

E,terna )orces Erosion De%osition

Historica Mi,t're


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Think a*o't %ro"inent !eat'res that yo'Think a*o't %ro"inent !eat'res that yo'

o*ser$e #ithin Indonesian Isand and theo*ser$e #ithin Indonesian Isand and the

s'rro'ndin& ocean !oor s'rro'ndin& ocean !oor


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Geologic Time

Time is an important component ofgeology; this separates geology frommost other sciences

Man’s most ancient history extends back just thousands of years in time; events ingeologic time have occurred overmillions or even billions of years!


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Geologic Time There are two methods of geologic

dating: relative and absolute Relative dating involves sequencing of

geologic events Absolute dating provides specific dates

for rock units or geologic events


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SKA(A WAKTU #EO(O#I


66/76

zaman

masa

r ' e R " ' <

e r - " i r

e r a & i " + @

r a & i " + @

m u l a & i " +

STRATIGRA-H. / 0ORTH WEST 1A+A -LA. SUMMAR.

s e r - a & i " +


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S " u r

R e s e

S e a l

# e + e

M i $ r

A ' ' u m

PRODUCTIVE AREASTRATIGRAPHY

BASIN DATATECTONICS FACIES

FORAM ZONEBLOW (1960)

STAGEAGE

S H A L L O W M

A R I N E

S H A L L O W

M A R I N E

N E R I T

I C - L I T O R A L

S H A L L O W

M A R I N E

D E L T A T O

F L U V I A L

F L U V I A L

N O N

M A R I N E

C I S U 2 U H

- A R I G I

C I 2 U L A K A 0

A T A S

2R)

T A L A 0 G A K A R

+ O L C 3

1 A T I 2 A R A 0 G

PASIRJADI

SUBANG TUGU

GANTAR CICAUH

TANJUNGSARI

SU!AMANDI

TUNGGULMAUNG

TUGU

SINDANG

PEGADEN

BOJONGRAONG

TUGU TAMBUN

!HB CLS

CILAMAYA UTARA

!HT CILAMAYA

TIMUR

CILAMAYA UTARA

WANAJAYASU!AMA

NDI

CEMARA

JATIBARANG

SR " SOURCE ROC!

R " RESERVOIRSL " SEAL

P L E I S T O

C E N E

P L I O C

E N E

P r e s

M I D

E A R

L Y

L A T E

E A R L Y

L A T E

L A T E

WIDE S-READ

COM-RESSIO0

U-LI)T /

EROSSIO0

SAG -HASE

-OST RI)T

RI)T E0DS

S.0RI)T

GRA2E0 )ILL

4EARL. S.0RI)T5

RI)TI0G

COMPILED BY IRZ-IND

M I O C E N E

O L I G O C E N E

E O C E N E


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To In$esti&ate Geoo&ica Settin&To In$esti&ate Geoo&ica Settin&


69/76

& & && & &

o! the Eastern Indonesia6663o! the Eastern Indonesia6663


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-ORO0G TOURIST A0D S-A -OTE0TIAL0 t -h ) i t S i ti t d T i t


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T8o!ou 8$ en o ,$e , ,t t8e u 7o$c,noe-

0at'ra-heno"ena )ascinate Scientists and To'rist


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7"t" "leh 9iji Press( T"ru Eamanaka(T"shi*umi

Kitamura$A7P$!ett, mages#el( 5 Mar 2%18


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kuliah geologi dasar kelas a 2014-2015 1&2

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