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RG - Kinta Valley-Tertiary Rock

Total questions: 25

Worksheet time: 15mins

Name
Class
Date
1.

Choose the correct statements about Kinta Valley

a)

limestones are evidently shelf-type and coralline types

b)

passes laterally eastwards into strata of the Baling Group

c)

fauna suggest warm water environments from the Silurian to Permian in the Kinta Valley

d)

a possibility of a depositional break due to uplift and erosion during the Palaeozoic

2.

The lithology of KL Area is

a)

schists, phyllites, quartzites, some volcanics and rare limestone occur

b)

thick Silurian limestone overlain by Upper Paleozoic (?) mudstone- sandstone sequence

c)

thick limestone predominate ( Silurian – Permian)

3.

In Kinta Valley, the oldest known sediments to be deposited appears to be

a)

schists, phyllites, quartzites, some volcanics and rare limestone occur

b)

carbonaceous argillaceous rocks of the Ordovician which may later be metamorphosed to black schists

c)

thick Silurian limestone

4.

The absence of clastic sediments in Kinta Valley suggest that

a)

the area was some distance from land or neighbouring land was of low relief

b)

continuous deposition of limestone

c)

No evidence of Devonian earth movements

5.

Choose the correct statement about Kinta Valley

a)

shales form homogenous & low hills with relief

b)

Clastic sedimentary rocks are found in southwest part of the Kinta Valley (Seri Iskandar)

c)

Interbedded sandstone & mudstone strike nearly N-S & have very steep dip angle

d)

All of the above

6.

KL area composed of 4 rock formations;

a)

Dinding Schist

b)

Kenny Hill Formation

c)

KL Limestone

d)

Hawthorndon Schist

e)

Karak Formation

7.

What is the thickness and lithology of Dinding Schist

a)

1830 meters of Upper Silurian marble

b)

3400 m of quartz-mica schist, quartzite and subsidiary actinolite, diopside and epidote schist and schistose conglomerate

c)

900 meters of non-fossiliferous carbonaceous schist and phyllite

d)

Quartzite forms a discrete member 1770 m thick in the middle of the succession

8.

The age fo Dinding Schist has been reassigned to

a)

Lower Paleozoic based on mapping

b)

Lower Silurian

c)

Upper Silurian

9.

Hawthorndon Schist has the lithology of

a)

Interbedded sandstone and mudstone

b)

quartz-mica schist, quartzite and subsidiary actinolite, diopside and epidote schist and schistose conglomerate

c)

900m non-fossiliferous carbonaceous schist and phyllite

10.

Which is incorrect about Hawthorndon Schist

a)

passes conformably up into the thick Upper Silurian KL Limestone

b)

Unit overlies a thick sequence of psammitic and pelitic schist

c)

Age Lower Ordovician

d)

May be a southern continuation of the Mahang Formation

11.

What is the thickness and lithology of KL Limestone

a)

900 meters of non-fossiliferous carbonaceous schist and phyllite

b)

1830 meters of Upper Silurian marble

12.

KL Limestone is located at

a)

Damansara area

b)

northern end of Klang Valley – Batu Caves

13.

Choose the correct statements about KL Limestone

a)

Richly fossiliferous in some horizons

b)

Overlie a thick sequence of carbonaceous schist and phyllite

c)

Marble is fine crystalline, grey to cream , thick bedded

d)

All of the above

14.

Fossils that can be found in KL Limestone are

a)

tentaculites

b)

corals

c)

brachiopod

d)

crinoids

15.

What are the differences between Kenny Hill Formation and KL Limestone

a)

Kenny Hill Formation is simper and different structural pattern from KL Limestone

b)

Kenny Hill Formation is younger than KL Limestone

c)

Kenny Hill Formation is older than KL Limestone

16.

Why is Kenny Hill Formation is on unstable shelf?

a)

lack of very coarse material in sand and high mineralogical maturity

b)

Presence of deformational structures and evidence of re-sedimentation

c)

Possible presence of brachiopods indicating not very shallow marine water

d)

dominance of well rounded zircons in heavy mineral

e)

all of the above

17.

Which formations are similiar to Kenny Hill Formation giving its probable age of Upper Paleozoic to Carboniferous?

a)

Singa Formation

b)

Kubang Pasu Formation

c)

Chuping Formation

18.

What is the possible contact found in Kenny Hill Formation

a)

Low angle thrust fault found in Damansara

b)

reverse fault found in Damansara

c)

Horst graben fault found in Damansara

19.

Boring in Malacca and N. Sembilan revealed 2 major stratigraphic units which are

a)

arenite and psammitic schist

b)

restricted calcareous

c)

Argillite and pelitic schist

20.

Which statement is incorrect

a)

Outcrops of Bentong can be traced Southwards through East N. Sembilan to Malacca

b)

Kenny Hill Formation extended to N. Sembilan

c)

Early Devonian rocks have not been proven in Selangor-Melaka area

21.

Which describes the stratigraphic argillite unit found in Malacca and N. Sembilan

a)

quartz sandstone and siltstone metamorphosed to schistose sericite and chloritic meta-quartzite, sillimanite and garnet bearing schist and gneiss

b)

fine-grained silty beds with minor sandy, shaly and marly bands with subordinate arenaceous beds and occasionally chert and conglomerates

22.

In the Western Belt, Triassic rocks can be found in which formation?

a)

Kenny Hill Formation

b)

Semanggol Formation

c)

Karak Formation

23.

Choose the correct statements about Triassic rocks in Western Belt

a)

Have turbidite characteristics

b)

underlies a sequence of probable post-Triassic redbeds unconformably

c)

contacts between the Semanggol and older formations are interpreted to be folding

d)

marine Triassic arenaceous and argillaceous rocks with chert bands

24.

Why was there no Triassic sediments known in the tract of Western Belt from Kinta Valley southwards?

a)

uplift probably preceded by deformation could have been initiated in the late Permian as the youngest known sediment is mid-Permian

b)

due to uplifting during Triassic

c)

erosion and upilft after Triassic

d)

all of the above

25.

The Tertiary rock found in Western Belt are represented by

a)

small basinal rocks of shale and other clastics with coal bands

b)

arenaceous and argillaceous rocks with chert bands