2. GEOLOGY AND TECTONIC OF
CHAMMAN FAULT
Members;
Abdul Majeed Bughio
M.A Dahri
Shazan Qureshi
Assigned By;
M.Afzal Jamali
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3. CHAMAN
Chaman چمن) is the capital of Qilla Abdullah
District, Balochistan Province, Pakistan. It is
situated just south of the West-Chaman
border crossing with the
neighbouring Kandahar
Province of Afghanistan. After the
capital Quetta, Chaman is the second-
largest city and tehsil in
the Pashtun majority northern part of
Balochistan Province.
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5. CHAMAN FAULT
The Chaman Fault is a major,
active geological
fault in Pakistan and Afghanistan that
runs for over 850 km.
Tectonically, it is actually a system of
related geologic faults that separates
the Eurasian Plate from the Indo-
Australian Plate.
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8. 8
It is a terrestrial, primarily transform, left-
lateral strike-slip fault. The slippage rate along the
Chaman fault system as the Indo-Australian Plate
moves northward (relative to the Eurasian Plate)
has been estimated at 10 mm/yr or more
9. In addition to its primary transform aspect, the
Chaman fault system has a compressional
component as the Indian Plate is colliding with the
Eurasian Plate.
This type of plate boundary is sometimes called a
transpressional boundary.
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10. From the south, the Chaman fault starts at the triple
junction where the Arabian Plate, the Eurasian Plate and
the Indo-Australian Plate meet, which is just off
the Makran Coast of Pakistan.
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11. The fault tracks northeast
across Balochistan and then north-northeast
into Afghanistan, runs just to the west
of Kabul, and then northeastward across the
right-lateral-slip Herat fault, up to where it
merges with the Pamir fault system north of
the 38° parallel.
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12. The Ghazaband and Ornach-Nal
faults are often included as part of
the Chaman fault system. South
of the triple junction, where the
fault zone lies undersea and
extends southwest to
approximately 10°N 57°E, it is
known as the Owen Fracture
Zone.
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15. While there is general agreement
that the fault is slipping at a rate of
at least 10 mm/yr, there is a report
of volcanic rocks in Pakistan
dated to 2 m.y. BP which have
been offset such as to indicate a
slip rate of 25–35 mm/yr.
Offsets have been described
throughout the fault in Pakistan
that are young enough that “only
the alluvium of the bottom of
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16. The parallel mountain ranges of
eastern Balochistan, (east to west)
the Kirthar Mountains, the Khude
Mountains, the Zarro Mountains, the
Pab Mountains and the Mor
Mountains, are a result of the
compressional plate boundary and are
aligned parallel to the Chaman fault
movement. The fault itself is west of
these ranges.
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17. OTHER FAULTS IN PAKISTAN
Main Karakoram Thrust.
Riasi Thrust.
Salt Range Thrust.
Bannu Fault.
Quetta-Chiltan Fault.
Allah Bund Fault.
Hoshab Fault.
Makran Coastal Fault
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19. MAJOR EARTHQUAKE PRODUCE BY CHAMMAN FAULT
On September
2013, a 7.7
magnitude earthqua
ke was recorded
along a fault
associated with
the Chaman
fault system in
southern Pakistan.
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20. CONCLUSION
Rupture initiated at the southern tip of the Chaman Fault and
propagated along the Hosbah fault within the Makran
accretionnary prism
Large strike-slip motion (6m on average, along 200km long
fault trace, 0-12km depth) on pre-existing thrust fault
Strike-slip enhanced due to eastward squeezing of Makran
prims
No shallow slip deficit
Large rupture velocity on
misoriented fault
Rupture failed to propagate along
the Chaman fault (despite most
aftershocks there).