2 edition of ...Miocene Foraminifera from Sumatra and Java, Netherlands East Indies found in the catalog.
...Miocene Foraminifera from Sumatra and Java, Netherlands East Indies
Leslie Walter Le Roy
1944 in Golden, Col .
Written in English
|Statement||by L.W. Le Roy...|
|Series||Quarterly of the Colorado school of mines,, v. 39, no. 3|
|LC Classifications||TN210 .C68 vol. 39, no. 3|
|The Physical Object|
|Number of Pages||113|
|LC Control Number||44042524|
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Get this from a library. Miocene Foraminifera from Sumatra and Java, Netherlands East Indies book East Indies.
[L W LeRoy] Paragloborotalia siakensis (LeRoy).—Spezzaferri and Premoli Silva,pl. XI, figs. 2a-c Miocene foraminifera from Sumatra and Java, Netherlands East Indies, part 1. Miocene foraminifera of central Sumatra, Netherlands East Indies.
?taxon=Paragloborotalia siakensis&module=pf_cenozoic. LeRoy, L. (b). Miocene foraminifera from Sumatra and Java, Netherlands East Indies, part 1. Miocene foraminifera of central Sumatra, Netherlands East Indies. Colorado School of Mines Quarterly.
39(3): gs. LeRoy, L. (a). Miocene foraminifera from Sumatra and Java Netherlands East Indies, part 2. Small foraminifera from the ?taxon=Sphaeroidinella multiloba&module=pf_cat. Some small foraminifera ostracoda and otoliths from the Neogene (Miocene) of the Rokan-Tapanoeli area, central Sumatra.
Natuurk. Tijdschr. Nederl.-Indie. 99(6): gs. LeRoy, L. (b). Miocene foraminifera from Sumatra and Java, Netherlands East Indies, part 1. Miocene foraminifera of central Sumatra, Netherlands East ?taxon=Dentoglobigerina baroemoenensis&module=pf. The biostratigraphic ranges of identified larger benthic and planktonic foraminifera from Tertiary exposures in East Java Basin have been tied to the ages constrained from the Strontium isotope Depositional Environment of the Batuasih Formation on the Basis of Foraminifera Content: A Case Study in Sukabumi Region, West Java Province, Indonesia June DOI: /ijog.v7i systematic paleontology of oligocene-miocene planktonic foraminifera from ne libya Article (PDF Available) June with Reads How we measure 'reads' The evolution of Lepidocyclina (L.) Isolepidinoides, L.
(Nephrolepidina) Nephrolepidinoides sp nov., L. (N.) Brouweri and L. (N.) Ferreroi in the late Oligocene-Miocene of the Far East Indonesia Main Page: Indonesia's History and Background.
Sukarno, Indonesia's founding president ANCIENT TIMES. Indonesia did not exist as yet during the Palaeocene period (70 million years BC), the Eocene period (30 million years BC), the Oligacene period (25 million years BC) and the Miocene period (12 million years BC) Ages OF Miocene fossil localities in the northern Kutai basin (East Kalimantan, Indonesia) Article (PDF Available) in Palaios 30(1) February with Reads How we measure 'reads' Miocene foraminifera from Sumatra and Java, Netherlands East Indies, Netherlands East Indies book 1.
Miocene foraminifera of central Sumatra, Netherlands East Indies. Colorado School of Mines Quarterly. 39(3): gs. Globigerinoides sacculiferus irregularis compiled by the [email protected] project team viewed: 8 ?taxon=Globigerinoides sacculiferus irregularis.
Renema, W., c, Comment on “Significant Miocene larger foraminifera from South Central Java” by M.K. Boudagher and S.W. Lokier, Revue de Paléobiologie – Google Scholar Renema, W., in press, the internal architecture of the miocene Pseudotaberina and REFERENCES. Akers, W.H., Some planktonic foraminifers of the American gulf coast and suggested correlations with the Caribbean Tertiary.
olibanum of Java), corrupted in the parlance of Europe into benjamin and benzoin; camphor, produced by Cinnamomum Camphora, the "camphor laurel" of China and Japan, and by Dryobalanops aromatica, a native of the Indian Archipelago, and widely used as incense throughout the East, particularly in China; elemi, the resin of an unknown tree of the Philippine Islands, the elemi of old writers being Netherlands East Indies between andwhich methodical survey, the results of which have been published in the Explanations to the Geol.
Map of Sumatra, scale 1: 1), in a certain way may be considered as a continuation of the explorations Boudagher-Fadel MK, Lokier SW () Significant Miocene larger foraminifera from south central Java. Revue de Paléobiologie – Google Scholar Buzas MA, Culver SJ () Understanding regional species diversity through the log series distribution of :// East Java is the easternmost part of Java Island.
Four principal physiographic zones of Java Island were first identified as structural units by van Bemmelen () and subsequently adapted and described by Whitten et al.,Lokier, as northern alluvial plains, northern foothills and plains, central volcanic mountains and southern mountains (or a southern dissected plateau and plains) ().
(Geological overview map of the Netherlands East Indies. First geological overview map of Indonesia, xcm, commissioned by Netherlands Royal Geographical Society. Java and Sumatra rel. complete map, but much of Kalimantan, Sulawesi and New Guinea still mostly uncharted territory) Abendanon, E.C.
()- Aequinoctia, an old Palaeozoic Paleobathymetric trends of Neogene foraminiferal assemblages and sea floor tectonism in the Andaman Sea area. Marine Geol., Three Miocene and two Pliocene samples recovered from the floor of the Andaman Sea indicate a tectonic history for the sea floor which is VLERK, ISAäK MARTINUS VAN DER(b.
Utrecht, Netherlands, 31 January ; d. was no more than an expedient to meet the needs of field geologists engaged in the systematic survey of the isles of Java and Sumatra. Six subdivisions based on larger foraminifera were distinguished, Tertiary a—f.
“Oligo-Miocene Lepidocyclinas and ('The paleontology and stratigraphy of Netherlands East Indies'.
Commerative volume at 80st birthday of Prof. Martin. Voluminous book with 20 chapters summarizing ˘state of knowledge ˇ of paleontology and stratigraphy in Netherlands East Indies.
With listings of species and fossil localities and stratigraphic :// Small foraminifera from the Miocene of West Java, Netherlands East Indies.
Quarterly Colorado School Mi 3, p. (Descriptions of species of small benthic foraminifera from Miocene marls at Tjijarian bridge, E of Pelabuhan Ratu, W Java) Lokier, S.W. ()- Volcaniclastic controls on carbonate sedimentation within the Gunung Literature sources used for this study included reports by the Mining Service of the Netherlands East Indies and private Dutch companies (–), oil industry reports (mostly post), and maps and reports prepared by the Geological Survey of :// 1.
Introduction. Modern equatorial carbonate production is most prolific in the clear shallow-waters of Southeast Asia and almost half the world's coral reefs and the greatest species diversity of corals occurs in this area (cf.
Umbgrove,Salm and Halim,Tomascik et al., ).Carbonate production was also extensive in the shallow-marine seas of Southeast Asia during the Cenozoic Abstract: Well‐preserved, isolated specimens of Pseudotaberina were found at three localities in Indonesia, thus enabling the study of the relationships between this genus and Caribbean Archaiasinae.
The internal architecture of the chambers of Pseudotaberina consists of four layers of stolon planes, each of which is divided by superposed septula into :// The primary goal of my research is to unravel the Cenozoic to Recent evolution of coral reefs in the Indo-Pacific.
To achieve this goal, I rely on a thorough understanding of the ecology and evolution of large benthic foraminifera. These small calcifiers are an important component of the coral reef carbonate budget, and were even more so in the :// Foraminifera from the Middle Eocene in the southern part of the Netherlands province of Limburg.
p., 10 figs, 13 pls, 1 folding table, paperbound; PI € 24 Bellen, R.C. van, Foraminifera from the Middle Eocene in the southern part of the Netherlands province of Limburg.
p., 10 figs, 13 pls, paperbound (lacking folding tables Turbidite play is productive in North Sumatra, East Java and offshore Kalimantan, but under explored in East Java.
Miocene carbonate play, productive in West Java and NE Sulawesi. Pliocene clastic play which consists of fluvio-deltaic sandstones and turbidites, proven as main oil and gas producers in Kutei and Tarakan basins in East Welcome to the new New features include: Split screen display — allows users to scroll the journal article and the article figures simultaneously; Faceted searching — added facets for journal, journal section, article type, book series and GeoRef keywords; Integrated OpenGeoSci Map view search results — allows users to limit search by geographic location Biostratigraphy of the Late Miocene Halang Formation in the Loh Pasir succession, Banyumas, Central Java – M.
Hendrizan et al. 32 Indonesia Micropaleontological education in –H. Darman 77 A revision of the biostratigraphy and strontium isotope dating of Oligocene-Miocene outcrops in East Java, Indonesia – E.
Sharaf et al. 44 Bering benthic forams Neogene benthic foraminifera from the southern Bering Sea (IODP Expedition ) On some foraminifera from the Microzoic deposits of Trinidad, West Indies. Proceedings of the Zoological Society of London, LeRoy, L.W.
Miocene foraminifera from Sumatra and Java, Netherlands East Indies. Colorado Cambridge Core - Palaeontology and Life History - Ecology and Applications of Benthic Foraminifera - by John W.
Murray The Pemali Formation can be correlated to other phases of accelerated clastic sedimentation across Java following widespread mid-Late Miocene tectonism. In eastern Java the equivalent is the Ledok to Mundu succession (cf. Marks, ) and to the south-east it is most East Indies, Indonesia, &c., is the vast congeries of islands which lie between south-eastern Asia and northern Australia.
This archipelago is usually taken to include 1. The Great Sunda Islands Java, Sumatra, Borneo, and Celebes, with islands adjacent to them or Ijdng between them.: 2. The Philippine The Moluccas. :// Globigerina baroemoenensis.
Citation: Globigerina baroemoenensis LeRoy Rank: species Type locality: Locality Ho, meters S° W. of kampong Kassikan, Tapoeng Kir i area, Rokan-Tapanoeli Region (approximately between north latitudes 0°30' and 1°50' and east longitudes 99°40' and °30'), Central Sumatra, Netherlands Indies; auger hole sample, depth 6 ?taxon=Globigerina baroemoenensis&module=pf_cat.
DIRECTOR’S FOREWORD (Daniel Pauly). Historical Ecology of the Raja Ampat Archipelago, Papua Province, Indonesia. ABSTRACT. INTRODUCTION. The spice trade and the East Indies.
Explorations in New Guinea. Oceanographic and marine biological studies. MATERIALS. The Study Site: Kepulauan Rajaampat (Raja Ampat Archipelago). Marine biodiversity. METHODS. Biodiversity of marine Full text of "Catalogue of the fossil Foraminifera in the collection of the British Museum (Natural History) Cromwell Road, S.W." See other formats Using fossils to tell geological time, biostratigraphy balances biology with geology.
In modern geochronology - meaning timescale-building and making correlations between oceans, continents and hemispheres - the microfossil record of speciations and extinctions is integrated with numerical dates from radioactive decay, geomagnetic reversals through time, and the cyclical wobbles of the earth.