Title: Lecture 8a: Stratigraphy, Paleomagnetism
1Lecture 8a Stratigraphy, Paleomagnetism
- Questions
- How is stratigraphy related to analysis of
sedimentary environments? - What happens when sea-level varies?
- How do variations in the terrestrial magnetic
field get recorded in rocks and used by
geologists to reconstruct history? - Reading
- Grotzinger et al. chapters 8 (again) and 14
2Principles of Stratigraphy (revisited)
- Recall the fundamental principles of
stratigraphy original horizontality,
superposition, cross-cuttting - A more detailed study brings up three major
themes - Uniformitarianism the interpretation of ancient
deposits by analogy to modern, observable
environments - Cyclicity climate, sea-level, annual, tidal
variations, etc., all generate repeating cycles
of sedimentation - Hierarchy basic stratigraphic principles apply
across a wide range of space and time scales - Definitions of stratigraphic elements Rock units
are organized into a hierarchy of classifications
There are also supergroups and subgroups, used
when original group definitions later prove
inadequate to describe important associations.
3Stratigraphydefinitions
- The boundaries between rock units can be
conformable or unconformable. - Conformable is meant to describe continuous
deposition with no major breaks in time or
erosional episodes. This definition is somewhat
scale-dependent just how long or large a gap is
an unconformity depends on the size and time
significance of the units being divided. - A vertical succession of strata represents
progressive passage of time, either continuously
at the scale of observation (conformable) or
discontinuously (unconformable). - A lateral succession of strata represents
changing environments of deposition at the time
of sedimentation or diagenesis. - Each recognizable environment in a lateral
succession is called a facies.
4Stratigraphydefinitions
- Unconformities are usually divided into four
types - Angular unconformity is used when layers below
are clearly tilted or folded and then eroded
before deposition continues on the eroded surface
- Disconformity is used when beds above and below
are parallel but a well-developed erosional
surface can be recognized, by irregular incision,
soil development, or basal gravel deposits on
top. - Paraconformity is used for obscure unconformities
where correlation with time markers elsewhere
indicates missing strata, even though no evidence
of a gap is present locally. - Nonconformity is used for deposition of bedded
strata on unbedded (usually igneous or
metamorphic) basement.
5Stratigraphydefinitions
- Any package of sedimentary strata bounded above
and below by an unconformity (of any kind) is a
sequence. - Traditional sedimentology and stratigraphy judge
formations to be the fundamental units of the
rock record, and interpretation of sedimentary
environments to be the essential product of
stratigraphic studies. - Sequence stratigraphy makes sequences the
fundamental units of the rock record, and hence
emphasizes periods of deposition and
nondeposition (closely related to episodes of
rising and falling sea level) as the essential
information. Sequence stratigraphy grew out of
seismic stratigraphy unconformities are easily
distinguished in seismic records, but lithology
is often unknown. - Sedimentary accumulation (hence the boundaries of
sequences) is controlled by changes in base
level, the elevation to which sediments will
accumulate if the local land surface is too low,
or erode is the local land surface is too high.
6Stratigraphy Base Level
- On land, base level is set by the equilibrium
profile of river systems. - In marginal marine settings, base level is often
the same as sea level - In the deep sea there is no base level and
sedimentation is controlled only by sediment
supply. - Changes in base level allow the sedimentary
record to preserve evidence of geological events - Relative sea level change is the most important
determinant of changes in base level. - Local tectonic uplift or subsidence changes base
level and leads to erosion or accumulation. - Changes in water supply or sediment load affect
the equilibrium profile of a river and therefore
the base level downstream.
7Stratigraphy Base Level
- On land, base level is set by the equilibrium
longitudinal profile of river systems, which
evolve to a characteristic shape
The parameters of the curve for each river are
different, and depend on various parameters.
Changes in these parameters will cause the river
to aggrade or incise to reach a new equilibrium
base level. Parameters include the elevation of
the headwaters, which may change by uplift or
erosion the elevation of the mouth, which may
change up uplift or sea-level change the
sediment supply, the water discharge, the type of
rock being cut.
8Stratigraphy Base Level
A knickpoint (resistant bed or lake) where the
form of the river is interrupted leads to a
nested set of river profiles.
The placing of an artificial knickpoint in a
river by building a dam has curious consequences,
both upstream and downstream. A waterfall must
retreat because it is steeper than the
equilibrium gradient for the reach of the river
below the falls. A sudden drop in base-level
leads to the formation of river terraces
9Stratigraphy Relative Sea Level
- Relative sea level is the depth of water relative
to the local land surface. - Relative sea level can change due to local
vertical tectonic motions or due to eustatic sea
level variations (i.e. global changes in the
volume of ocean water or of the ocean basins). - In both sequence and traditional stratigraphy,
the critical events that determine the locations
of environments and unconformities are
transgressions and regressions. - A transgression is a landward shift in the
coastline, and hence a landward shift in all
marginal marine environments. A regression is a
seaward shift in the coastline. - A drop in relative sea level always causes a
regression. A transgression hence requires rising
relative sea level. However, rising sea-level
can result in transgression, stationary
shorelines, or regression depending on sediment
supply. - This asymmetry results because sediment flux from
land is always positive, and because
transgression during sea-level fall would create
unstable, over-steepened long-valley profiles.
10Stratigraphy Relative Sea Level
- rising sea-level can result in transgression,
stationary shorelines, or regression depending on
sediment supply.
- Whether transgression or regression occurs
controls the preservation potential and vertical
succession of environments like barrier islands
11Stratigraphy Walthers Law
- We are now ready to state the third fundamental
tenet of traditional stratigraphy, lateral
continuity, which is expressed by Walthers Law - In a conformable vertical succession, only those
facies that can be observed laterally adjacent to
one another can be superimposed vertically - That is, if the lateral shifting of sedimentary
environments is controlled by continuous changes
in base-level, each point accumulating sediments
vertically passes through all intermediate
environments continuously. - Thus, e.g., deep-sea sediments directly overlying
a terrestrial flood-plain facies demands an
unconformity in between. - Consider again the vertical succession of beach
facies, which maps the lateral succession of
beach facies onto a single point as the beach
progrades outwards during a regressive relative
sea-level rise.
12Stratigraphy Transgression and Regression
- In vertical succession, transgression is
recognized by progression from inland towards
deep water sediments moving up section
regression, if preserved, is recognized by
progressively shallower water facies moving
towards continental settings as you go up section.
13Stratigraphy Transgression and Regression
On a regional-continental scale, transgression is
recognized by lateral migration of environments
with time, from the coast towards the interior,
and regression by migration of environments
towards the coast.
The ideal sequence consists of a transgressive
clastic formation, a carbonate formation
deposited when essentially the whole continent
was flooded, and a regressive clastic formation
(less often preserved after erosion).
14Sequence Stratigraphy
On a continental scale in North America, there
are recognized six major transgressions and
regressions, bounded by five major regional
unconformities. These sequences were named in
North America by Sloss (1963), but they correlate
fairly well with patterns seen on other
continents. They are therefore interpreted as
major changes in eustatic sea level, not as
continental-scale uplift and subsidence.
15Sequence Stratigraphy
- Superimposed on the major Sloss sequences are
second-order cycles of transgression and
regression usually called Vail curves, and
superimposed on these are third-order cycles that
are correlated with individual reflectors in
seismic sections of marine strata. Tracing and
correlating these sequences is the main project
of sequence stratigraphy. - Repeated transgressions and regressions,
presumably related to cyclic rises and falls of
sea level, lead to cyclic sedimentation episodes
in sedimentary basins. In particular, the
Pennsylvanian strata of the eastern U.S. show at
least 50 distinct cylcothems consisting of the
triplet of deposits marine-fluvial-coal. Each is
a regression, probably caused by withdrawal of
water from the oceans during a glacial advance.
16Causes of sea-level change
- Relative sea level can change due to local or
regional tectonics, which cause vertical motions
(uplift and subsidence). Global sea level can
only change by altering either the volume of sea
water or the volume of the ocean basins
themselves. - On time scales of 103105 years, glaciation can
quickly tie up and release enough water to change
global sea level by 200 m. But Sloss cycles have
time scales of 108 years and amplitudes of 1000
m! - Changes in the global configuration of continents
and the working of plate tectonics can affect
global sea level by changing the volume of the
oceans - when continents are assembled into
supercontinents, the area of shallow shelves is
greatly decreased and the mean age of the ocean
crust is a maximum, because there are few small
oceans and one big one. This should lead to a big
fall in sea level (Permian through Jurassic
regression?). - when continents rift, a new, shallow ocean is
created at the expense somewhere of an old, deep
ocean. Sea level should rise. - an increase in spreading rate of the global
ridge system leads with time to increase in the
volume of water displaced by the mid-ocean ridges
and a sea-level rise (cause of Cretaceous
transgression?).
17Paleomagnetism
- As we have already discussed, the Earths
magnetic field varies with time and records of
the paleomagnetic field are preserved in rocks.
Lets look in more detail. - Magnetization of rocks
- At high temperatures, all materials are
paramagnetic, meaning their magnetization is
proportional to the applied field, and zero in
the absence of an applied field - Materials with unpaired electron spins can
undergo a phase transition to ferromagnetic
behavior at a temperature called the Curie Point.
- A magnetic mineral crystallized above the Curie
point and then cooled through it acquires a
thermal remanent magnetism (TRM) in the same
direction as and with intensity proportional to
the applied field.
18Paleomagnetism
- If a magnetic mineral is formed by chemical
alteration or metamorphism at temperatures below
its Curie Point, it acquires a chemical remanent
magnetism. If a given rock cooled at one time
with some magnetic minerals and was altered later
to grow new magnetic minerals, the TRM and CRM
may point in different directions. - They can be separately measured by progressive
demagnetization of a sample with increasing
temperature. - If magnetic particles are eroded from a source,
transported, and deposited in a new rock under
appropriate conditions, all below the Curie
Point, they will have a preferred orientation
governed by the magnetic field at the time of
sedimentation, a depositional remanent magnetism.
This will typically be 1000 times weaker than
the magnetic moment in a lava where each little
dipole is perfectly aligned, but it is measurable.
19Paleomagnetism
- Measurement of the vector remanent magnetic field
in a rock sample gives the declination and
inclination of the field at the time and location
of acquisition. - If the terrestrial magnetic field was a simple
dipole at the time of acquisition, this
measurement gives a virtual magnetic pole - The declination gives the orientation of the
great circle on which the pole lies, and the
inclination gives the magnetic latitude of the
sample.
20Paleomagnetism
- A measured virtual magnetic pole reveals several
facts - Magnetic polarity at time of magnetization,
assuming you know which hemisphere the sample was
in and have some rough idea of horizontal - Intensity of the field at the time of
magnetization, if you correct for the
susceptibility of the particular sample.
21Paleomagnetism
- The apparent latitude of the sample at the time
of magnetization. If it does not match the
present latitude, you can infer that the sample
has moved north or south. - There are terranes on the west coast of North
America whose magnetic inclinations imply motions
of thousands of kilometers. - You get no information on longitude, which is a
limitation in the reconstruction of positions of
continents in the past this is particularly
serious before the Mesozoic, when there are no
marine magnetic anomalies to go by. - Tectonic rotations about a vertical axis show up
through anomalies in the measured declination. - A sequence of virtual magnetic poles from a
series of rocks of different ages attached to one
stable continent defines an apparent polar wander
(APW) path. - Apparent because it is not clear without a
fixed frame of reference whether it is the
continent or the pole that has wandered. - However, the difference between APW paths for two
different continents gives an accurate
measurement of the relative motion between the
two continents.