Ditemukan 1106 dokumen yang sesuai dengan query
Kuala Lumpur: Department of Museums Malaysia, 2014
748.209 595 ANC
Buku Teks SO Universitas Indonesia Library
New York: Fleming H Revel Co., 1947
808.8 QUO
Buku Teks SO Universitas Indonesia Library
Kuala Lumpur: Persatuan Sejarah Malaysia, 1980
913.926 PER l
Buku Teks SO Universitas Indonesia Library
Jakarta: Departemen Pendidikan dan Kebudayaan RI, 1989
899.224 4 BUJ
Buku Teks SO Universitas Indonesia Library
Bartlett, John
Boston Little, Brown and Company 1955
RB 808.88 B 38 f
Buku Referensi Universitas Indonesia Library
Shalihin Damiri, N.
Sidoarjo: Balai Bahasa Provinsi Jawa Timur, 2021
889.223 43 SHA b
Buku Teks Universitas Indonesia Library
Rahmah Bujang
Kuala Lumpur: Dewan Bahasa dan Pustaka. Kementerian Pendidikan Malaysia, 1989
782.1 RAH s
Buku Teks SO Universitas Indonesia Library
"Archaeological sites of Pengkalan Bharu, Perak is one of the important ports in Malaysia. The port is associated with the center of the Government of New Beruas. Establishment of the port city is to anticipate the enemy like a pirate attack of siam, Aceh, Maja-pahit, selangor and Portuguses."
Artikel Jurnal Universitas Indonesia Library
Yuniarti Ulfa
"Nenering Formation is essentially made up of semi-consolidated sediments, which are divided into basal conglomerate beds, conglomeratic sandstone, cross-bedded sandstone, and siltstone to muddy layers facies. It is overlie unconformable to the Berapit Formation, but conformable to the Kroh and Grik Formations. The stratigraphy of Nenering Formation is a fining upwards sequence where the thickness of conglomerate beds become thinner upwards and become thicker for conglomeratic sandstone. The thickness varies from 0.5 m to tenths of meters. The more sandy in the upper portion (cross-bedded sandstone) overlie with thin siltstone and mudstone facies. The clast and grain composition suggested that the material making up the sedimentary sequence were derived predominantly from the erosion of granitoid rocks and sedimentary and metamorphic rocks constitute a minor provenance. Imbrications and the trend sizes of clasts indicate that the palaeo-current flow toward northeast. Cross bedding that was found in conglomerate and sandstone indicates the main channel depositional environment. The sequence stratigraphy of this area match with the Saskatchewan fluvial braided channel model."
Pusat Teknologi Bahan Galian Nuklir. Badan Tenaga Nuklir Nasional, 2014
660 EKSPLOR 35:2 (2014)
Artikel Jurnal Universitas Indonesia Library
Jakarta: Pusat Pembinaan dan Pengembangan Bahasa, Departemen Pendidikan dan Kebudayaan, 1991
899.224 4 IND s (1)
Buku Teks Universitas Indonesia Library