II- Formation of Tarim Basin. 1. A context of collision. 2. A sedimentary basin. 3. Retreat of .... landscape evolution along the Keriya River, Xinjiang, China: the.
The Tarim Basin formation of an endorheic basin and its climatic consequences Laurie Bougeois M1 PSP
Introduction General geology : a context of collision between the Indian Plate and the Eurasian Plate
Tarim Basin
Mettre une photo montrant rapidement la collision et situant le bassin du tarim. Cf livre le choc des continents
Outline I- The elements of Tarim Basin 1.
The Taklamakan : an endorheic desert
2. The boundary mountains 3.
Main rivers and lakes
II- Formation of Tarim Basin 1.
A context of collision
2. A sedimentary basin 3. Retreat of Paratethys Sea 4. Desertification and aridification III- Tarim Basin and origins of transition of paleoenvironnemental patterns 1.
Uplift of Tibetan Plateau
2. Retreat of Paratethys Sea
3. Which phenomenon is the main responsible?
I- The elements of Tarim Basin 1. The Taklamakan : an endorheic desert Surname : « The desert of Death »
Climate : very arid and big range of temperature : -40°C < T < +50°C Area : 337 000 km² => 3rd bigger desert in the world
Dunes of sand : up to 40m of hight (end of formation : 70ka ago)
Formation of desert : Miocene with the retreat of an epicontinental sea (Paratethys)
I- The elements of Tarim Basin 2. The surrounding mountains
Tian Shan : northern border
Composition : mainly crystalline
and sedimentary rocks of the
Paleozoic Era (540 - 250 Ma)
n Sha lun n u K
Orogenesis during Late Eocene
Highest peak : Victoria Peak
(7439 m)
I- The elements of Tarim Basin 2. The surrounding mountains
Kunlun Shan : southern border
Principal folded structures and
granitic rocks date to 250 Ma
Sedimentary cover : until
Jurassic
n Sha lun n u K
Orogenesis 26 Ma ago
Highest peak : Kunlun Goddess
(7167 m)
I- The elements of Tarim Basin 2. The surrounding mountains
Pamirs : western border
Formed by junction of the Tian
Shan, Karakoram mountains, Kunlun Shan and Hindu Kush ranges
(7495 m)
n Sha lun n u K
Highest peak : Ismoil Somoni
I- The elements of Tarim Basin 3. Main rivers and lakes a. Hydrological settings : An endorheic basin
Lots of rivers but only one go through the desert of Taklamakan
I- The elements of Tarim Basin 3. Main rivers and lakes b. Keriya River :
Takes its origin in the Kunlun Shan and finishes with a delta in the sand
Keriya river
I- The elements of Tarim Basin 3. Main rivers and lakes b. Keriya River :
Takes its origin in the Kunlun Shan and finishs with a delta in the sand
c. Khotan River :
Go through the Taklamakan (from South to North)
Khotan and Keriya rivers
I- The elements of Tarim Basin 3. Main rivers and lakes d. Tarim River :
Go along the North of Taklamakan Confluence = union of Asku, Khotan and Yarkand
Longest river in the basin : {Yarkand+Tarim} = 2030 km
I- The elements of Tarim Basin 3. Main rivers and lakes e. Lop Nor :
End of Tarim River
Group of small salt lakes and marshes in a depression
Area = 10 000 km² but decreases for several centuries
II- Formation of Tarim Basin 1. A context of collision Remains of a microcontinent :
Turan
Collision between the Turan Plate and the Eurasian Plate during Carboniferous and Permian
II- Formation of Tarim Basin 1. A context of collision Remains of a microcontinent :
Turan
Collision between the Turan Plate and the Eurasia Plate during Carboniferous and Permian
II- Formation of Tarim Basin 1. A context of collision Remains of a microcontinent :
Turan
Collision between the Turan Plate and the Eurasia Plate during Carboniferous and Permian
II- Formation of Tarim Basin 1. A context of collision
Since
between Plate
Lots
Paleogene
Indian Plate
of
:
and
deformations
borders of the basin
collision
Eurasian
in
the
=> consequences of the thrust of Tian Shan and Kunlun Shan over the basin
II- Formation of Tarim Basin 2. A sedimentary basin Sedimentation in the basin of Paratethys Sea (extended across the Eurasian continent during the Eocene)
II- Formation of Tarim Basin 2. A sedimentary basin Paleogene Sediments - Permian mudstones – Precambrian shield Accumulation of the most of sediments on the southeastern border (basin in slope)
Big reservoir of oil and natural gases but which has lost its waterproofness because of tectonic movements
II- Formation of Tarim Basin 3. Retreat of Paratethys Sea Retreat of Parathetys 30 Ma ago
II- Formation of Tarim Basin 3. Retreat of Paratethys Sea Remains of Parathetys =
Caspiane Sea and Aral Sea
II- Formation of Tarim Basin 4. Desertification and aridification Since the retreat of Parathetys : desertification and aridification during Late Miocene
Formation of big dunes of sand Lots of evaporation
Today drought still increases and basin totally surrounded, closed
III- Tarim Basin and origins of transition of paleoenvironnemental patterns Two hypothesis for aridification in North and season of monsoon in South and the Eocene-Oligocene transition (34 Ma)
1. Uplift of Tibetan Plateau Changes in the atmospheric circulation ➔ ➔
aridification to the North (Tarim basin) monsoon to the South
Uplift and orogenesis = erosion ➔
consumption of CO2 and climate changes
Positive feedback between uplift and erosion
III- Tarim Basin and origins of transition of paleoenvironnemental patterns Two hypothesis for aridification in North and season of monsoon in South and the Eocene-Oligocene transition (34 Ma)
2. Retreat of Parathetys sea Before the retreat : ➔ ➔
stopped warming of Central Asia
decreased the development of monsoon in the South
After the retreat : ➔
great aridification of Tarim basin
III- Tarim Basin and origins of transition of paleoenvironnemental patterns Two hypothesis for aridification in North and season of monsoon in South and the Eocene-Oligocene transition (34 Ma)
3. Which phenomenon is the main responsible? Impact of uplift of Tibet
Paratethys part is about as important as the Tibetan plateau part BUT : ➔
uplift of Tibetan plateau =
Impact of Paratethys
localized effect, no big
changes in big scale ➔
retreat of Parathetys =
regional impact and more significant
Conclusion Tarim basin : an interesting basin for geologists formation in a big context of collision
understanding of phenomenon of endorheism
origin of one part of aridification and environnemental changes like the climate monsoon-dominant predict and anticipate climate changes
Tarim basin : an interesting basin for industrialists and politics a big reservoir of oil ( nearly 15 billions of tons if it is still waterproofness) and gases (70%=methane) Lop
Nor : lots of nuclear testing
predict and anticipate climate changes
References Articles : X. Yang et al. Late Quaternary palaeoenvironment change and landscape
evolution
along
the
Keriya
River,
Xinjiang,
China:
the
relationship between high mountain glaciation and landscape evolution in foreland desert regions. INQUA. 2002
Neil and Houseman. Geodynamics of the Tarim Basin and the Tian Shan in Central Asia. 2007. Tectonics.
Z.
Zhongshi
et
al.
What
triggers
the
transition
of
palaeoenvironmental patterns in China, the Tibetan Plateau uplift or the Paratethys Sea retreat ? 2007. PALAEO
E.
Sobel.
Basin
analysis
of
the
Jurassic–Lower
Cretaceous
southwest Tarim basin, northwest China. ANNEE ET REVUE???
P. E. Rumelhart et al. Cenozoic vertical-axis rotation of the
Jul 11, 2009 - (the last quadratic part of the equation being neglected), such that the temperature variations may be used to trace the seasonality. 4.
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