Lecture 2 Flashcards

1
Q

beds to sedimentary basins

A

lithostratigraphy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

biozones and stratigraphic ranges

A

biostratigraphy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

reversals and polarity chrons

A

magnetostratigraphy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

LOWESS 87Sr/86Sr ratio curve

A

chemostratigraphy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

orbital eccentricity cycles

A

cylcostratigraphy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

igneous rocks such as granites formed from melts deep underground (–) or above ground in the form of lavas and tuff (volcanic rocks)

A

plutonic

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

metamorphic rocks such as slate, marble, and gneiss formed by – and another kind of rock

A

heating and/or squeezing

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

examples of sedimentary rock

A

shales and sandstones

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

sedimentary rock are formed of materials transported by water and/or wind and deposited in areas of –

A

low potential energy (sedimentary basins)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

– is concerned with the order of deposition of sedimentary rocks

A

stratigraphy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

lithostratigraphy involves the recognition of – which are features on geological maps

A

rock units

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

sedimentary rocks are deposited in layers called –

A

bed or laminae

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

– consist of a succession of similar beds or an alternation of two or a few different types

A

rock units

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

basic rock unit

A

formation

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

fromations may lie on continents (epicontinental) or at the edges of the continents or –

A

sea floor

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

sea floor spreading followed by – limits the age of ocean basin deposits to less than about 150 Ma

A

subduction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

T/F: 300 Ma Australia was much farther south

A

true

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

Nowra Sandstone is resistant to erosion so it’s a – sandstone

A

cliff forming

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

longshore drift causes quartz to move – along the Burdekin River

A

northward

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
20
Q

total duration of any taxon from first to last individual is called the –

A

biozone

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
21
Q

best estimate of a biozone is the – which is normally less than the biozone

A

stratigraphic range

22
Q

the Earth’s magnetic field periodically – every 10^5 or 10^6 years

A

reverses

23
Q

the present situation with the – in the Arctic is normal

A

north pole

24
Q

times between reversals called – is instantaneous

A

chrons

25
Q

chemostratigraphy uses secular (time) changes in – as indication of elapsed time

A

chemical tracers

26
Q

abrupt changes (–) in chemostratgraphic records enable events to be correlated locally and globally

A

excursions

27
Q

typical tracers are – such as 13C/12C, 18O/16O, 34S/32S, 87Sr/86Sr

A

ratios of stable isotopes

28
Q

– are used for global correlation because the ocean is homogeneous on long timescales

A

strontium isotope ratios

29
Q

there are two principal inputs of strontium to the ocean: Whole-Earth values (light) derived from seafloor volcanic rocks and –

A

continental crust (heavy)

30
Q

most metronomic cycles are driven by astrophysical processes such as the rotation of the Earth, orbit of the Earth around the sun, variations in the Earth’s obliquity, precession of equinoxes, and –

A

eccentricity of the orbit

31
Q

Milankovitch first linked cyclical changes in Earth’s orbital elements to –

A

climate

32
Q

Cyclostratigraphy: fossils and sediments record environmental changes as – in the thickness and composition layers

A

variations

33
Q

if the – of the cycle is known then cyclostratigraphy may be used to date past events

A

frequency

34
Q

in the Denver basin, there are ash beds (“little dudes”)above and below the – boundary dated to 66Ma

A

K-T

35
Q

Eons: Hadean, Archean, Proterozoic, and

A

Phanerozoic

36
Q

the Precambrian (pre-Phanerozoic) most boundaries are defined by – clock dates

A

arbitrarily chosen

37
Q

In the Phanerozoic most boundaries reflect – in the fossil assemblages first recognized during the 19th century

A

successive changes

38
Q

Some boundaries such as the K-T coincide with –

A

natural events

39
Q

Some boundaries such as the – have marginal natural significance

A

S-D

40
Q

GSSP stands for

A

Global Stratotype Section and Point

41
Q

GSSP is also known as

A

Golden Spikes

42
Q

GSSP reduce the four dimensions of space and time to a –

A

single point

43
Q

T/F: GSSPs are selected by international working groups appointed by the IUGS Commissions on Stratigraphy

A

true

44
Q

T/F: National competition for GSSPs is fierce like World Heritage sites as they attract visitors and funding

A

true

45
Q

GSSPs mark the – of time intervals

A

beginnings

46
Q

Ediacaran GSSP defines the terminal period of the –

A

Neoproterozoic

47
Q

Ediacaran GSSP follows the –

A

Cryogenian

48
Q

Ediacaran was placed at the interface between the – and the post glacial cap carbonate

A

last major glacial sediment

49
Q

Ediacaran GSSP is located in

A

Enorama Creek, South Australia (2004)

50
Q

Ediacaran GSSP is about – Ma

A

635