Zobrazeno 1 - 10
of 19
pro vyhledávání: '"C. J. Pigram"'
Autor:
D. J. Blundell, H. Prasetyo, A. J. Barber, S. Tjokosaproetro, A. Richardson, C. J. Pigram, D. B. Snyder
Publikováno v:
Tectonics. 15:34-53
New deep seismic reflection profiles across the Banda Arc of Indonesia reveal reflectors in the uppermost 50 km of the lithosphere. Combined with existing earthquake hypocenter locations and focal mechanisms, the new structural geometries inferred fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f77083a1001faf29ff44c019f782dbfb
https://doi.org/10.1029/95tc02352
https://doi.org/10.1029/95tc02352
Publikováno v:
Reefs and Carbonate Platforms in the Pacific and Indian Oceans
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6ec98b63e324fe7d12438a741e525078
https://doi.org/10.1002/9781444304879.ch8
https://doi.org/10.1002/9781444304879.ch8
Publikováno v:
Global and Planetary Change. 3:341-361
The characteristics of carbonate facies deposited along continental margins are directly controlled by seawater temperature. The oxygen isotopic composition of foraminifera tests reflect seawater temperature, and accordingly isotopic and age data may
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9f224998fba2665f70790bcdf89054e9
https://doi.org/10.1016/0921-8181(91)90116-e
https://doi.org/10.1016/0921-8181(91)90116-e
Publikováno v:
Proceedings of the Ocean Drilling Program, 133 Scientific Results
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f73ac4a8e50bf639127531ab8fb563fc
https://doi.org/10.2973/odp.proc.sr.133.271.1993
https://doi.org/10.2973/odp.proc.sr.133.271.1993
Publikováno v:
Proceedings of the Ocean Drilling Program, 133 Scientific Results
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad0663d77c1d1449b4499cd357bd86cd
https://doi.org/10.2973/odp.proc.sr.133.250.1993
https://doi.org/10.2973/odp.proc.sr.133.250.1993
Middle Miocene carbonates of the Marion Plateau consist of dolomitized bioclastic floatstones and rudstones with rhodoliths (up to 6 cm in size) as the most prominent component. These rhodoliths are embedded in a bioclastic matrix with Halimeda, echi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b17a4341a91cacacb464f72785224d65
https://doi.org/10.2973/odp.proc.sr.133.244.1993
https://doi.org/10.2973/odp.proc.sr.133.244.1993
Publikováno v:
Geology. 20:858
The Miocene carbonate platform of the Marion Plateau in northeast Australia preserves an excellent record of sea-level fluctuations. The warm-water platform consists of an early to middle Miocene second-order highstand complex, whereas the late Mioce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed78a53ff408ac9499cdb696393bf8c9
https://doi.org/10.1130/0091-7613(1992)020<0858:amotso>2.3.co
https://doi.org/10.1130/0091-7613(1992)020<0858:amotso>2.3.co
Autor:
Hermes Panggabean, C. J. Pigram
Publikováno v:
Nature. 301:231-234
The age of the Banda Sea is critical for palaeogeographical reconstructions of eastern Indonesia. Assumed ages for its formation range from Mesozoic to Neogene1–10. However, geophysical evidence shows that the Banda Sea is floored by oceanic crust1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ff347a9f7118e88f35bbff0bdaf40eb
https://doi.org/10.1038/301231a0
https://doi.org/10.1038/301231a0
Publikováno v:
Marine and Petroleum Geology. 5:75-81
Six major seismic stratigraphic sequences in the Raggatt Basin on the southern Kerguelen Plateau overlie a basement complex of Cretaceous or greater age. The complex includes dipping reflectors which were apparently folded and eroded before the Ragga
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3751a632cbb75c7dd271756c152a0350
https://doi.org/10.1016/0264-8172(88)90041-4
https://doi.org/10.1016/0264-8172(88)90041-4
Publikováno v:
Nature. 296:556-558
The island of New Guinea, geologically and structurally part of the Indian–Australian plate1,2, is shown on continental reconstructions of the Permian globe as forming the northeastern part of the supercontinent of Gondwana3,4, facing a large Tethy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::603db5ff55ec755c1a9c327fb7fe3f3c
https://doi.org/10.1038/296556a0
https://doi.org/10.1038/296556a0