CLASSIFICATION CLASSIFICA TION OF PLUTONIC ROCKS Minerals and mineral groups: Q quartz A alkali feldspars (orthoclase, microcline, perthite, anorthoclase, albite) P Plagioclse, scapolite F feldspathoids or foids (leucite and pseudoleucite; nepheline, sodalite, nosean, hauynite, cancrinite, analcime, etc.) M mafic and related minerals (micas, amphiboles, pyroxenes, olivines, opaque minerals, accessories (zircon, apatite, tianite,etc), epidote, allanite, garnets, melilites, monticellite, primary carbonates, etc.) Q +A + P = 100 100 or A + P F = 10 100 0
Succession of Minerals in Rock Names (all rock types): Descriptive nomenclature should appear in order of most abundant mineral to least abundant mineral.
CLASSIFICATION OF VOLCA NIC ROCKS VOLCANIC Q
BROAD CLASSIFICATION OF IGNEOUS IGNEOU S ROCKS BY COLOR A N D G R A I N S I Z E
0-90 volume % mafic minerals 60
For example: a granodiorite containing more biotite than hornblende is a “biotite-hornblende granodiorite”.
ROCKS WITH M<90%
alkali feldspar rhyloite
rhyolite
alkali feldspar 20 trachyte 5 trachyte Latite A 10 35 65 10 p h o n o l i t e
dacite
alternatively: andesite: M: 0-35% basalt: M 35-90%
andesite (SiO2>62%) basalt (SiO2<62%)
tephritic phonolitic phonolite thephrite
P
Tephrite: (OL 0-10%) basanite: OL > 10%)
% Dark Minerals 0-35% 0-3 5% Leu Leucoc cocrat ratic ic 35-65% Meso Mesocrati cratic c 65-90% Melan Melanocrat ocratic ic 90=% 90 =% Ul Ultr tram amaf afic ic Average Grain Size <1 mm -- fine grained 1-5 mm -- medium grained 5-30 mm -- coarse grained >30 mm -- pegmatitic
60 Q 6-20%: add prefix quartz F 0-10%: add prefix foid bearing
foidites
2 . . 1 V . . S F E R D L O G O L G N A
F Y P O C T O N O D
CLASSIFICATION CLASSIFICA TION OF PYROCLASTIC ROCKS
GLASS
Vitric Tuff, Ash Tuff,
GABBROIC ROCKS Crystal Tuff, Ash Tuff, CRYSTALS, CRYSTAL FRAGMENTS
Lithic Tuff, Ash Tuff, ROCK FRAGMENTS
TERMS USED FOR MIXED PYROCLASTIC-EPICLASTIC ROCKS ULTRAMAFIC ROCKS
Pyroclasts Volcanic + nonvolcanic epiclasts (+ minor amounts of biogenic, chemical sedimentary and authigenic constituents).
A N G L D O O G N O O L T D C R O E P S F Y . V 1 . 2
PARTICLE SIZE TERMINOLOGY
GRAIN ROUNDNESS AND SPHERICITY Y T I C I R E H P S Ve ry Ang ular
A ngul ar
S ub-a ngul ar
Su b-ro unde d
Rou nde d
Very Ro unde d
R O U N D N E S S
G R A I N
P E R C E N T A G E
1%
15%
2%
20%
2 . 1 V . S F E R D L O G O L G N A
Y P O C T O N O D
3%
25%
5%
30%
7%
40%
10%
50%
BEDDING THICKNESS TERMINOLOGY
A N G L D O O G N O O L T D C R O E P S F Y . V 1 . 2
2 . 1 V . S F E R D L O G O L G N A
Y P O C T O N O D
C I T A E R H P
a i c c e r b n o i t p u r E
f o s n r o e i t t a a s w i r l u a s m s r e e r h p t e o e D g
s m w r o o f l f l t a u i o c r i f e r t n u i S s
C I T A M G A M O T A E R H P
a i c c e r b d e z i d i a u i l c f c x e i r r b t a e m m d e e r l t l a l i i D M
d i p a r s d r e n t a a s w e l i t d a n u l o o v r g f f o o g g n n i t i t n a e e V h
s t n e e v r u e d t m e c u e i z r r t d t s a i i u s l d f t i e i x l o t r p a t i x d a e e m a d i m r l e c c e l t e i r n M b I
C I T A M G A M
a i c c r s e e b p l i p a a m r i e c h c t e r o r b d c y i n h c a i c t l o a v - m s b g e p u a i S M p
e m a N n o m m o C
n i o f i o s u n t r o n i t i u l o m o s r x f e s t l e n i e t a l l o o i V v
n i g i r O
l e v e l y r y h t n p r e o v p t t o a n p d e e e e D N
l e v e L
d e s o p x e e n o N
r e v l i e s - t i l d c i r o g e l s - a a i m r r a e l h u i t d p A e
s e m o d s u o n e g o d n E
r d l e o p g - p l o a c - t d e l m o e g s n a o t b - i a e i d t f a l n u o s b r h g a i C H
s e k i d , d e v i r e d - y r y h p o r P
e v y i i s t v u i r t t n c I a
e t i s a c e r n a i f - m a / e c t i i l r i y S p
s e p i p g n d i r e f p f p t u a h d s - n a s e t e n n i o e c a C v f
r a , l d u e g v n i r a e y d l y n o l l a m c m o o L c
e t i r y p - a c i l i S
e e t i t i n c f e e t i d m e r s t y p a o n e t i n i e l t l i m t a c e i s r s s r e i y S D c
e m e r t e a i m d e r t n i a i h t s d i e f w i o s c a t e f u i c g o a i n n f r w t f n f o e u r V T h t
i l d c l i t i l e s p i i a l r l m e y r l n t a l i o c i r n w s a o a i u r h t e r t e a n c r i s s t c e c e l n a t i n e l i s e m a i f n g c f o u u a r L J f T
d e d z e i d r i e u t l l f a d e t n i a r y d p e y - l l i l a M c
e t a n o / - b r = a d c l o o t g - g l d e i n o d d g - i f a l l a u r t s - g e z r , m t e r p e a p s u o a Q c b
r t e a o p d s z i t r d l p a f e e u - , e q - K t l e , i t e o i i i c t n i r t o t c e i S B A
y s y b t n b d e d e m e t t a g a n a n i r i f m e m o v o d i d s s s s u e t r l e t l n y i n t t y e s d s m n e e g o c s a i r u p f s d a l u o l l a r r t t o c n i n C l o I
e s s e p l y a t l l s o n c o i n t i c s e j a i n i l c a c n i e c r o b s l t n d l e e n g a n m i g c h i a t s f r r m a d s a l e e g u l l l a b t y i a s M M t
n o i t a z i f l o a r e e l n y i t S m
n o i t a r e t l A
m r o F
s t n e m g a r F
e c p a s n e p o r , u o l f
k c o R
x i r t a M
A N G L D O O G N O O L T D C R O E P S F Y . V 1 . 2
) 1 8 9 1 , n a n a h c u B r e t f A
2 . 1 V . S F E R D L O G O L G N A
Y P O C T O N O D
( t i s o p e d l a m r e h t i p e l a t e m s u i o i c e r p ” l a c i p y t “ a n i n o i t a z i l a r e n i m o t d e t a l e r s t c e f f e n o i t a r e t l A
A N G L D O O G N O O L T D C R O E P S F Y . V 1 . 2
M E A S U R M E N T KNOWN
MULTIPLY BY
C O N V E R S I O N S
TO CALCULATE
KNOWN
LENGTH
TO CALCULATE
28.350 0.453 0.035 2.204
grams kilograms ounces pounds
CM
1
WEIGHT ounces pounds grams kilograms
Inches feet yards miles millimeters centimeters meters meters kilometers
2.540 30.480 0.914 1.609 0.039 0.393 3.280 1.093 0.621
centimeters centimeters meters kilometers inches inches feet yards miles
AREA 2 centimeters 2 sqmeters 2 meters 2 kilometers 2 inches 2 feet 2 yards 2 miles acers
0.155 10.7639 1.196 0.3861 6.4516 0.0929 0.8361 2.590 0.405
inches 2 feet 2 yards 2 miles 2 centimeters 2 meters 2 meters 2 kilometer s hectares
2
2 1 3
VOLUME fluid ounces pints quarts gallons (U.S.) Milliliters liters liters
29.573 0.473 0.946 3.785 0.033 1.056 0.264
milliliters liters liters liters fluid ouinces quarts gallons (U.S.)
4
2
5
TEMPERATURE °C = (° F - 32) x .555 °F = (° C x 1.8) = 32
6
DENSITY FOR COMMON ROCK TYPES
2 . 1 V . S F E R D L O G O L G N A
MULTIPLY BY
IN
7 3
DENSITY (g/cm )
MATERIAL
Y P O C T O N O D
In Place
3
After Excavation
8
9
4
10
11
SLOPE CORRECTION CALCULATIONS slopeº
distance (m)
run (m)
distance (m)
run (m)
distance (m)
12 run (m)
distance (m)
run (m)
5
5
50
50.19
100
100.38
150
150.57
200
200.76
10
50
50.77
100
101.54
150
152.32
200
203.09
15
50
51.77
100
103.53
150
155.30
200
207.06
20
50
53.21
100
106.42
150
159.63
200
212.83
25
50
55.17
100
110.34
150
165.51
200
220.68
30
50
57.74
100
115.47
150
173.21
200
230.95
35
50
61.04
100
122.07
150
183.11
200
244.14
40
50
65.27
100
130.55
150
195.82
200
261.10
45
50
70.71
100
141.42
150
212.13
200
282.85
13
14
6
15
16
17
A N G L D O O G N O O L T D C R O E P S F Y . V 1 . 2
GUIDLINES FOR COLORS BY GEOLOGIC AGE AND ROCK TYPE Stratified & Metamorphic Holocene Qh
C C I
O O Z
QUATERNARY Q
Upper u
z O C
Z N
Pliocene Tp Miocene Tm
TERTIARY T
E C Lower l
O
Pleistocene Qp
Oligocene To Eocene Te Paleocene Tl
R
2 . 1 V . S F E R D L O G O L G N A
E Y P O C T O N O D
C I O Z O M S E M
N
A
C I O Z z O P
H E
P
L A P
CRETACEOUS K
Upper u Lower l
JURASSIC J
Upper u Middle m Lower l
TRIASSIC TR
Upper u Middle m Lower l
PERMIAN P
Upper u Lower l
CARBONIFEROUS C
N A I R B A C E R P
Acid
Intermediate
Basic
Acid
Intermediate
Basic
Upper u Lower l
ORDOVICIAN O
Upper u Lower l
CAMBRIAN C
Upper u Middle m Lower l
s k c r o o R l c i a n s a s c y l o b V a p y H
s k c r o o R c l i n a s o s t y u b l P a p y H
Utramafic
Acid
Basic
SILURIAN S
ARCHEAN A
Igneous
Intermediate
Upper u Middle m Lower l
O Z O R P L E T O R P
Upper u Lower l
DEVONIAN D
C C p I
Undifferentiated
Acid
Intermediate
Basic
Utramafic
s k c r o o R c l i n a a s c s y l o b V a p y H
s k c r o o R c l i n a s o s t y u b l P a p y H
A N G L D O O G N O O L T D C R O E P S F Y . V 1 . 2