• Tidak ada hasil yang ditemukan

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

N/A
N/A
Protected

Academic year: 2017

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

Copied!
11
0
0

Teks penuh

Loading

Gambar

Fig. 1. (a) Geologic map of the Yarlung–Zangbo Suture Zone, southern Tibet, modified after BGMRT (1993), and the distribution of the Giabulin Formation, showing continental sutured characters between theLhasa Terrane (Asia) and the Himalaya Terrane (India)
Fig. 2. Sedimentary column of the Giabulin Formation showing characteristics of lithology, structures, paleocurrents, grain size changes, and distribution oflithologic units and environments
Fig. 3. Framework-grain QmFLt and QpLvLs composition (after Dickin-son, 1985) of the Giabulin Formation sandstones, mainly showing transi-tional-lithic recycled and subduction complex sources
Fig. 4. (a) Field photograph of the conglomerate within the Giabulin Formation showing rounded peridotite pebbles, and (b) back scattered electronphotomicrograph of chromite in peridotite clast.
+5

Referensi

Dokumen terkait

Because volcaniclastic sediments are absent in the adja- cent, structurally underlying crustal and mantle sequences (the ophiolite component) of the Neyriz ophiolite complex, we

40 Ar/ 39 Ar data from a pro®le across the Main Central Thrust in the eastern Bhutan Himalaya indicate muscovite cooling ages of 14.1..

A crustal shear zone in the interface zone between the Higher and Lesser Garhwal Himalaya with considerably high P-wave velocity and pronounced seismic activity is identi®ed. In

The tectonic events recorded in the Cretaceous accretion- ary–collision complexes in central Indonesia are subduc- tion, accretion of fragments of an oceanic plate and

[r]

together with comparable island arc terranes now found in Papua New Guinea and the Philippines, are interpreted to have formed part of a roughly east±west intraoceanic island arc

The Lesser Himalaya in central Nepal consists of Precambrian to early Paleozoic, low- to medium-grade metamorphic rocks of the Nawakot Complex, unconformably overlain by the

They are: (i) the Santonian±Campanian episode (86±77 Ma) represented by volcanic and plutonic rock exposures in the Masu Complex in Eastern Sumba; (ii) the