III.
Deep Sea Sediments (50 Points).
(20 points) A.
Terrigenous Sediments.
1.
Compare and contrast turbidites and contourites in terms of their
origin, sediment structures, and their geographic distribution. (10 pts.)
2. Briefly describe the possible origins for submarine canyons
and cite evidence supporting each possibility. (10 pts.)
(10 points) C.
Briefly describe the characteristics of cosmogenous sediments in the
deep sea, including their morphology, their distribution, their age, their
implications and their usefulness.
(20 points) B.
The sedimentary sequence on the left was drilled at a depth of 5700
meters in the western Pacific off the Japan Trench by the Glomar
Challenger. Briefly explain the
origin of this sedimentary sequence in terms of the factors controlling
biogenous sedimentation in the deep sea, subsidence of ocean crust, and
sedimentation rate.
A. The
sedimentary sequence on the left was drilled at a depth of 3800 meters west of
Bermuda in the Atlantic by the Glomar Challenger. Bermuda is an atoll sitting on top of a
seamount constructed in middle Eocene time (~45 m.y. ago) on crust of late
Jurassic (~150 Ma) age. In turn,
this seamount sits in the middle of a large swell called the Bermuda Rise,
which apparently was uplifted at the time the seamount formed. Assuming that the CCD in the North
Atlantic has been at a depth of 4500 meters since the late Jurassic (which is
not true), and assuming that ocean crust that is 30 Ma old lies at a depth of
4500 meters (which is true), briefly explain the origin of this sedimentary
sequence in terms of the factors controlling biogenous sedimentation in the
deep sea, evolution of continental margins, and subsidence of ocean crust. Use diagrams if you wish. (25 pts)
B. Also answer the following questions
concerning the sequence above. (20
pts)
1. What is the color and probable composition of the clay in the interval from 1150-1250 meters? Briefly explain the reasons for your answers.
2.
Sketch the sequence of sedimentary structures that would be found at
1000 meters. Label your sketch
with letters usually used for the various sections of the sequence. What is this sequence called?
A. The
sedimentary sequence on the left was drilled at a depth of 5000 meters in the
western south Atlantic off Brasil by the Glomar Challenger. Briefly explain the origin of this
sedimentary sequence in terms of the factors controlling carbonate
sedimentation in the deep sea, subsidence of ocean crust, and the evolution of
continental margins. (10 pts.)
A. The sedimentary sequence on the left
was drilled at a depth of 6500 meters east of Japan in the Pacific by
the Glomar Challenger on crust of late Jurassic (~150 Ma) age. Assuming that
the CCD everwhere in the Pacific except along the Equator has been at a depth
of 4500 meters since the late Jurassic (which is not true), and assuming that
ocean crust that is 30 Ma old lies at a depth of 4500 meters (which is true),
briefly explain the origin of this sedimentary sequence in terms of
sedimentation rates, the factors controlling biogenous sedimentation in the
deep sea, subsidence of ocean crust, and plate motions. Use diagrams if you
wish.
B. Also
answer the following questions concerning the sequence above. (20 pts)
1. What
is the color and probable origin of the clay in the intervals from 575-625
meters and from 375-425 meters?
Briefly explain the reasons for your answers.
2. How
would this section appear in a seismic reflection profile?