Apparent Polar Wander Path from the Tarim Block in China |
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作者姓名: | Robert Sharps Michael McWilliams |
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作者单位: | Geophysics Dept. Stanford Univ.,Stanford,CA94305,Geophysics Dept.,Stanford Univ.,Stanford,CA94305 |
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摘 要: | The apparent polar wander (APW) path from the Tarim block consists of palaeo-magnetic poles ofDevonian (λ=16°N, ψ= 165° E. A_(95)=4°). Late Carboniferous (λ=41° N, ψ=160° E, A_(95)=4°).Permian (λ=61°N, ψ=177° E. A_(95)=9°). Early Triassic (λ=69° N. ψ=183° E. A_(95)=11°) andJurassic/Cretaceous (λ=65° N, ψ=214° E. A_(95)=6°) times. On the basis of this APW path, it is con-cluded that the Tarim block was subducted beneath the Kazakstan plate between Devonian and Permiantimes. The Tarim, North China and South China blocks were sutured between the Early Triassic and EarlyCretaceous. Tarim had moved eastward some 2000 km relative to Siberia since the Cretaceous.
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Apparent Polar Wander Path from the Tarim Block in China |
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Authors: | Li Yanping Robert Sharps Michael McWilliams Zhang Zhengkun Li Yong' an Li Qiang Zhai Tongjian Gao Zhenjia |
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Abstract: | Abstract The apparent polar wander (APW) path from the Tarim block consists of palaeo- magnetic poles of Devonian (λ = 16 ° N, φ= 165 ° E, A95 = 4 °), Late Carboniferous (A = 41 ° N, φ= 160 ° E, A95 = 4 °), Permian u = 61 ° N, φ=177° E, A95 = 9°), Early Triassic U = 69° N, φ=183° E, A95=ll °) and Jurassic/ Cretaceous (A = 65 ° N, (A = 214 ° E, A95 = 6 °) times. On the basis of this APW path, it is concluded that the Tarim block was subducted beneath the Kazakstan plate between Devonian and Permian times. The Tarim, North China and South China blocks were sutured between the Early Triassic and Early Cretaceous. Tarim had moved eastward some 2000 km relative to Siberia since the Cretaceous. |
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