physiographic division of india(2)
5.
Gondawana
System. : -
a) Introduction -- After the deposition of
Vindhyan system there was a great period of non-deposition in the stratigraphy
of peninsula.
·
The name Gondawana comes from area of
south of Narmada by the Gondas were first studied.
·
It is made of deposition in the slowly sinking
faulted trough.
·
B]Distribution :- 1. A large tract in West
Bengal along Damodar valley & Rajmahal hills 2. along Mahanadi Valley 3. Along Godawari River & Penganga near
Nagpur 4
.Cutch, Rajasthan, Saurashtra, Wardha, Yeotmal, Nagpur, Chandrapur district of Maharashtra.
Classification:-
Upper Gondwana Umia fossil
Jabalpur tlyllophyllum flora
Middle Gondwana Rajmahal Da crodium flora
Mahadev
Panchet
Lower
Gondwana Damuda Raniganj [coal]
Barren measure
Barakar [coal]
Karharbari
Glossoptris & gongamopteris
Talchir
b) Lithology: - Shale, sandstone, conglomerate,
coal seam, intrusion of dolerite dyke.
c) Age:
- Carboniferous to Jurassic.
d) Indian coal:
- The economic importance of the Gondwana is that they are the major source
of coal in India. 80% of all coal comes from lower Gondwana [Damuda] i.e. both
in the Barakar & Raniganj series.
The important
coal fields in India are
1. Raniganj
coal field. 2.
Jhariya coal field. 3. Bokaro coal
field.
4. Rampura coal field. 5. Singareni coal field. 6. Giridih coal field.
Coal
field in Maharashtra: -
1. Kamtee coal field. 2.
Bokaro coal field.
3.Umrer
coal field. 4
Wardha coal field. 5 Ballarpur coal field
6 Ghuhus
coal field 7 Rajura coal field 8 Worora
coal field
6.
Deccan Trap :-
a) Introduction:
- At close of cretaceous period, large
part of peninsula was affected by volcanic activity. This result into a thick
series of lava pyroclastic material. Eruption of magma through fissures. Such type of eruption is called fissure type
of eruption .These flows are horizontal,
they look like flat plateau & their composition is basaltic so they are called plateau basalt.
They are called Deccan trap because of their step like appearance.
b)
Distribution: - 85% of area of Maharashtra & wide
area of M. P., Gujarat, A. P., Karnataka. Maximum thickness of lava 3000 mt.
c)
Lithology: - Plagioclase Augite basalt, Vesicular, compact,
Amygdaloidal basalt, Trachyte, Rhyolite, Andesite ,diorite gabbro.
d)
Types of basalt:-
1) Giant phenocryst Basalt. (2 to 10 cm) length of plagioclase.
2) Compact Aphanitic Basalt.
3)
Hydrothermal altered Basalt.
4) Amygdaloidal Basalt with large amygdales.
5) Amygdaloidal
Basalt with medium amygdales.
6) Amygdaloidal
Basalt with small amygdales.
7) Amygdaloidal
Basalt with pipe amygdales.
8) Vesicular Basalt.
9) Porphyritic Basalt.
10) Tachylytic Basalt (Red, green, black).
11) Red Tachylytic Basalt.
12) Volcanic
breccias
13) Volcanic breccias with gray lava matrix.
14) Volcanic breccias with R.T.B.
15) Volcanic
breccias with Zeolite matrix.
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