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Journal of Asian Earth Science

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

... The Ordovician Period closed with a glacial/glacio¯uvial event where the Ammar Formation terminated the Ordovi- cian System. Glaciers advancing north and northeastward from northern Arabia during the Late Ordovician ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... age of 113 ^ 3 Ma (mid-Cretaceous) (McCourt et al., 1996). To the north of Bandarlampung, spectacular exposures below an irrigation dam on the Sekampung River show extensive outcrops of granodioritic ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... Comparison of the basement compositions, pre-Devonian sedimentary features as well as the Palaeozoic palaeobio- geographic faunal and floral affinites of the Changdu-Simao and South China blocks ...part ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... hypothesis of the existence of a paleo-ophiolite is consistent with the sedimentary component of the Xigaze Group, and magmatism and volcanism on the Lhasa ...Formation of the Xigaze Group ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... Suturing of northern Australia to SE Asia takes place within a diffuse and still poorly understood region ...south of the Sunda Arc is marked by a deep trench, is replaced in the Banda Arc by a series ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... one of the best “natural laboratories” for the study of both extant and fossil ...assemblage of lithospheric continental blocks and the suture zones between them (representing former ocean basins), ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... part of the Sukhothai Fold Belt, the contact between the Lampang Group and Rong Kwang Formation is conform- able, indicating continuous deposition through the Permian–Triassic ...reports of continuous ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... part of the Kudi Ophiolite Complex, at the bridge approximately ...tion of the granodiorite is conspicuous in the field ...zone of unconsolidated sedi- ments (Fig. 6). The northernmost outcrop ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... geology of Cretaceous accretionary –collision complexes in central Indonesia is reviewed in this ...means of radiolarian biostratigraphy and meta- morphic petrology, as well as by geological ...results ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

... each of the three mutually perpendicular thin sections assuming the foliation plane as the XY plane and stretching lineation as the `X'-direction for each hand specimen collected across the MCT (Siddans, 1972; ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

... side of the ramp as a consequence of ramp development ...folds of Suppe and Medwedeff (1990). Development of more frontal ramps in an imbricate style under continued progressive shortening may ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:

... existence of seismic ...occurrence of a mainshock in a certain fault increases with the time elapsed since the occur- rence of the previous mainshock in this ...activity of small earthquakes ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... segment of the main Devonian to Middle Triassic Palaeo-Tethys ocean, and forms the boundary between the Gondwana-derived Sibumasu and Indochina ...result of northwards subduction of the Palaeo-Tethys ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

... framework of the Rajang Accretionary Complex is interpreted on the basis of field surveys conducted around the Lupar Fault Zone in southwestern ...series of thrust slices formed by accretion at a ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

... discussion of these alternative interpretations of Papua New Guinea is beyond the scope of this paper, but with reference to the latter interpretation, it is perhaps signi®cant that the Late ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

... observation of samples collected sys- tematically along two parallel sections ...intensity of deformation increases north- ward to the UMCT. Most parts of the Lesser Hima- laya lie within the ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

... N of Dasu and N of Duber Kale ...continuation of the Alpurai fault (Anczkiewicz et ...) of s 1 are attributed to late block tilting and/or to local vari- ations in stress ®eld ...S of ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

... sequence of a forearc basin which laps onto a ridge (Fortuin et ...position of the Sumba Ridge within the forearc since the initiation of the Sunda arc±trench system during the late Oligocene and the ...

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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue5.2000:

... intervals of the Wannienta basaltic magma, northern ...evolution of the residual magma with decreasing temperature show the following trends: At ...trend of the Kuanyinshan volcanic series is similar ...

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