definisi
marl iku sawijining rock sedimentary unconsolidated dumadi saka lempung lan jeruk
metapelite iku sawijining lapangan term geologi lawas lan saiki ora digunakake digunakake kanggo lempung sing sugih nggoleki-grained endhepan clastic utawa rock sedimentary, IE lendhut utawa mudstone a
asal
dingerteni
dingerteni
panemu
Dingertèni
Dingertèni
Etimologi
saka lawas marle french, saka pungkasan marglia latin
saka pelos utawa lempung ing Yunani
kelas
rocks sedimentary
rocks metamorphic
sub-kelas
awet rock, rock alus
awet rock, medium atose rock
group
ora ditrapake
ora ditrapake
kategori liyane
rock grained nggoleki, rock opaque
rock grained coarse, rock grained nggoleki, medium rock grained, rock opaque
werna
ibas, coklat, ijo, grey, putih
greenish peteng - werna abu-abu, ijo, ijo enom, klawu rodok ijo cahya
katon
atos lan kurang
banded
Efesus interior
aggregates hiasan, kothak lantai
aggregates hiasan, interior
Efesus njaba
minangka watu bangunan, kothak gendheng
minangka watu bangunan, minangka madhep watu
Efesus arsitektur liyane
curbing
curbing
industri construction
Pabrik semen, kanthi jumlah ongko construction, kanggo dalan kanthi jumlah ongko, nggawe semen alam, mentahan materi kanggo Pabrik mortir
Pabrik semen, kanthi jumlah ongko construction, kanggo dalan kanthi jumlah ongko
industri medical
durung digunakake
durung digunakake
Efesus jaman
artefak, perhiasan, reca, figurines cilik
artefak
komersial
nggawe kriya, kondisioner lemah
tablet commemorative, nggawe kriya
jinis
lempung marl, marl biru, marl abang, dhuwur marl bank, Nihan lapisan marl, ing lapisan Nihan marl, marl wedhi, marl ijo, marl werna abu-abu lan marl clayey
ora Sumadhiya
fitur
umume atos kanggo tutul, iku salah siji saka rock tuwa, splintery, rock grained banget nggoleki
gampang pecah dadi lancip piring, iku salah siji sing paling tuwa, kuat lan paling angel rock
monumen
durung digunakake
durung digunakake
monumen misuwur
ora ditrapake
ora ditrapake
reca
used
durung digunakake
patung misuwur
data ora kasedhiya
ora ditrapake
figurines
used
durung digunakake
tatanan
Wangun marl nalika partikel lempung banget nggoleki-grained sing setor ing banyu kang settles ing ngisor banyu badan lan compacted dening overlying endhepan; banyu meres metu lan Empu mbentuk rock marl.
amarga kanggo ngganti ing kondisi lingkungan, rocks sing digawe panas lan pressurized jero nang permukaan bumi. metapelite kawangun saka panas nemen disebabake magma utawa dening tabrakan kuat lan gesekan lempeng tektonik.
isi Mineral
kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz
albite, chlorite, quartz
senyawa isi
aluminium oxide, NaCl, cao, wesi (iii) oxide, silikon dioksida
aluminium oxide, cao, MgO
jinis metamorphism
ora ditrapake
ora ditrapake
jinis udan
udan biologi, udan kimia
udan biologi, udan kimia, udan mechanical
jinis erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi
ukuran gandum
banget nggoleki-grained
medium kanggo nggoleki coarse grained
rengat
conchoidal
fibrous
porosity
Highly keropos
Highly keropos
cleavage
ora kasedhiya
ora kasedhiya
kateguhan
2.6
ora kasedhiya
tartamtu gravitasi
2.2-2.8
3.4-3.7
Kapadhetan
2.4-2.8 g / cm 3
0-300 g / cm 3
kapasitas panas tartamtu
ora Sumadhiya
resistance
tahan panas, impact tahan
tahan panas, impact tahan, meksa tahan
celengan ing bawana wétan
asia
India, Pakistan, Russia
Not Yet Found
africa
Ethiopia, Kenya, Morocco, South Africa
Western Africa
europe
austria, france, germany, greece, italy, romania, Scotland, spain, Swiss
united kingdom
wong
durung ketemu
durung ketemu
celengan ing bawana kulon
lor amerika
USA
Not Available
kidul amerika
Colombia, Ecuador, Peru
Brazil, Colombia, Ecuador
celengan ing Oseania bawana
australia
New South Wales, Victoria, Western Australia
Central Australia, Western Australia