Zobrazeno 1 - 10
of 54
pro vyhledávání: '"R. Soeria‐Atmadja"'
Publikováno v:
Journal of Mathematical and Fundamental Sciences, Vol 8, Iss 2 (2019)
Busur Timur Sulawesi, yang terdiri dari Sulawesi Timur dan Tenggara, sebagian besar ditempati oleh suatu komplek luas terdiri dari kelompok batuan ultramafic yang diperkirakan berumur Mososoik hingga Tersier Bawah. Batuan-batuan tersebut dijumpai ber
Externí odkaz:
https://doaj.org/article/af57199173244fe397a63a78a10d19c3
Publikováno v:
Journal of Asian Earth Sciences. 18:533-546
The island of Sumba, presently located in the southern row of islands of the Eastern Nusa Tenggara province of Eastern Indonesia, has a unique position, being part of the Sunda-Banda magmatic arc and subduction system. It represents a continental cru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f19313ad3018ccf17a2098b34c979dd
https://doi.org/10.1016/s1367-9120(99)00082-6
https://doi.org/10.1016/s1367-9120(99)00082-6
Publikováno v:
Island Arc. 8:47-55
The Neogene Western Sulawesi Arc, from the south going northwards, can be divided into three magmatic provinces of K alkaline–shoshonitic (AK-SH), high-K calc-alkaline (KCA), and low-K–normal calc-alkaline (TH-CA) affinity, referred to, respectiv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f359da3412acd87968b62e4800344e7a
https://doi.org/10.1046/j.1440-1738.1999.00221.x
https://doi.org/10.1046/j.1440-1738.1999.00221.x
Publikováno v:
Journal of Asian Earth Sciences. 17:25-45
The NE–SW Tertiary magmatic belt of central Kalimantan is related to two separate periods of subduction; during the Eocene–Oligocene and Late Oligocene–Miocene. The younger magmatic belt is superimposed upon the earlier belt. This magmatic belt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::093bc724f65cbb2cc4e5a7f6bd2fdec4
https://doi.org/10.1016/s0743-9547(98)00062-2
https://doi.org/10.1016/s0743-9547(98)00062-2
Publikováno v:
Bulletin of the Geological Society of Malaysia. 42:257-268
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::789820be2f2d64421aa5b3b0617419ab
https://doi.org/10.7186/bgsm42199821
https://doi.org/10.7186/bgsm42199821
Publikováno v:
Journal of Asian Earth Sciences. 16:1-12
The western Sulawesi magmatic belt and the Sunda–Banda arc define the eastern and south-eastern margins of Sundaland, which is part of the relatively stable Eurasian plate. The eastern margin is bounded by the Makassar Strait which separates wester
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da275345eb124c2a084d7b85c1636cce
https://doi.org/10.1016/s0743-9547(97)00050-0
https://doi.org/10.1016/s0743-9547(97)00050-0
Publikováno v:
Journal of Southeast Asian Earth Sciences. 9:13-27
Evidence of the earliest magmatic event (Late Eocene-Early Miocene) has recently been discovered in East Java (Pacitan area) as exposures of pillow lava flows. Stratigraphically they represent the lowermost part of Besole Formation (Oligocene-Early M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::399bee3b2129e40d94fdc84a9e45c9c3
https://doi.org/10.1016/0743-9547(94)90062-0
https://doi.org/10.1016/0743-9547(94)90062-0
Autor:
Mireille Polvé, R Soeria-Atmadja, J. Cotten, Hervé Bellon, René C. Maury, Jean-Louis Joron, Bambang Priadi
Publikováno v:
Journal of Southeast Asian Earth Sciences. 9:81-93
40K-40Ar ages (27 new ones) and geochemical data (major and trace elements) allow the recognition of four main magmatic events in Central Sulawesi (South of Palu and in the Toraja area). The oldes magmatic activity took place during Late Eocene and O
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bc891c0a03dd2e4c940c346d2b4f2d24
https://doi.org/10.1016/0743-9547(94)90067-1
https://doi.org/10.1016/0743-9547(94)90067-1
Autor:
Hurbans, Nivriti1,2 9037508@stu.ukzn.ac.za, Naidoo, Panjasaram1
Publikováno v:
Pan African Medical Journal. Jan-Apr2024, Vol. 47, p1-12. 12p.
Publikováno v:
Bulletin of the Geological Society of Malaysia. 19:349-367
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5b143b83b4b87c9e9a39396bd2067ef
https://doi.org/10.7186/bgsm19198626
https://doi.org/10.7186/bgsm19198626