Theodore G. Th. Pigeaud and P. Voorhoeve. Handschriften aus Indonesien (Bali, Java, und Sumatra), xi, 71 pp., 6 plates. Stuttgart: Franz Steiner Verlag Wiesbaden GmbH, 1985. (Verzeichnis der Orientalischen Handschriften in Deutschland, XXVIII, 2.) DM 64,‐
G. J Knapp, Kruidnagelen en christenen: de Verenigde Oost‐Indische Compagnie en de bevolking van Ambon 1656–1696.xii, 323 pp. Dordrecht: Foris Publications, 1987. (Verhandelingen van het Koninklijk Instituut voor Taal‐, Land ‐en Volkenkunde, 125.) Guilders 35.
Rainer Carle (ed.). Cultures and societies North Sumatra. 514 pp. Berlin; Hamburg: Dietrich Reimer Verlag, 1987. (Veröffentlichungen des Seminars für Indonesische und Südseesprachen der Universität Hamburg, 19.) DM 95.
J. Noorduyn. Bima en Sumbawa: bijdragen tot de geschiedenis van de sultanaten Bima en Sumbawa door A. Ligtvoet en G. P. Rouffaer.xii, 187 pp. Dordrecht: Foris Publications, 1987. (Verhandelingen van net Koninklijk Instituut voor Taal‐, Land‐ en Volkenkunde, 129.) Guilders 30.
Anthony J. Whitten and others. The ecology of Sulawesi. By Anthony J. Whitten, Muslimin Mustafa, Gregory S. Henderson,xxi, 777 pp. Yogyakarta: Gadjah Mada University Press, 1987.
Robert Wessing. The soul of ambiguity: the tiger in Southeast Asia. vi, 148 pp. [Dekalb, Illinois]: Center for Southeast Asian Studies, Northern Illinois University, 1986. (Monograph Series on Southeast Asia, Special Report 24.) (Distributed by Cellar Bookshop, 18090 Wyoming, Detroit, Michigan 48221.)相似文献
A comparison of testamentary practice in medieval Genoa with that in Douai, France, reveals how differing social orientations resulted in profoundly contrasting social practices. Genoese society was chiefly privately orientated, and patrimony in Genoa was correspondingly transmitted along a vertical dimension. The public nature of the process in Douai, meanwhile, was correlated with a wide distribution of legacies on a horizontal axis. Women in Douai, therefore, enjoyed a scope of action not experienced by their Genoese counterparts. These circumstances, in turn, require a re‐evaluation of the so‐called ‘Frauenfrage‘ — the supposed problem of too many unmarried women. 相似文献
Transmigration in Indonesia, by J M Hardjono. Oxford in Asia Current Affairs. Kuala Lumpur: Oxford University Press 1977; xv, 116 pp, 8 maps, 15 tables. £6.00.
Myths and Legends of Indonesia, by Jan Knappert. Singapore: Heinemann Educational Books (Asia) Ltd, 1977; 198pp. £2.40. 相似文献
The Indonesian Tragedy by Brian May, London: Routledge & Kegan Paul, 1978, pp. xvii, 438. £8.95.
Comment fut tranchée la liane céleste, et autres textes de littévature orale bunaq (Timor, Indonésie), edited by Claudine Friedberg from the collection and translations of Louis Berthe, Paris: Société d'Études Linguistiques et Anthropologiques de France (Langues et Civilisations à Tradition Orale 25), 1978; pp. 294, 8 plates, 2 maps and several figures in the text. 相似文献
Permian hydrothermal activity in the Tarim Basin may have been responsible for the invasion of hot brines into Ordovician carbonate reservoirs. Studies have been undertaken to explain the origin and geochemical characteristics of the diagenetic fluid present during this hydrothermal event although there is no consensus on it. We present a genetic model resulting from the study of δ13C, δ18O, δ34S, and 87Sr/86Sr isotope values and fluid inclusions (FIs) from fracture‐ and vug‐filling calcite, saddle dolomite, fluorite, barite, quartz, and anhydrite from Ordovician outcrops in northwest (NW) Tarim Basin and subsurface cores in Central Tarim Basin. The presence of hydrothermal fluid was confirmed by minerals with fluid inclusion homogenization temperatures being >10°C higher than the paleo‐formation burial temperatures both in the NW Tarim and in the Central Tarim areas. The mixing of hot (>200°C), high‐salinity (>24 wt% NaCl), 87Sr‐rich (up to 0.7104) hydrothermal fluid with cool (60–100°C), low‐salinity (0 to 3.5 wt% NaCl), also 87Sr‐rich (up to 0.7010) meteoric water in the Ordovician unit was supported by the salinity of fluid inclusions, and δ13C, δ18O, and 87Sr/86Sr isotopic values of the diagenetic minerals. Up‐migrated hydrothermal fluids from the deeper Cambrian strata may have contributed to the hot brine with high sulfate concentrations which promoted thermochemical sulfate reduction (TSR) in the Ordovician, resulting in the formation of 12C‐rich (δ13C as low as ?13.8‰) calcite and 34S‐rich (δ34S values from 21.4‰ to 29.7‰) H2S, pyrite, and elemental sulfur. Hydrothermal fluid mixing with fresh water in Ordovician strata in Tarim Basin was facilitated by deep‐seated faults and up‐reaching faults due to the pervasive Permian magmatic activity. Collectively, fluid mixing, hydrothermal dolomitization, TSR, and faulting may have locally dissolved the host carbonates and increased the reservoir porosity and permeability, which has significant implications for hydrocarbon exploration. 相似文献
ABSTRACT Rapid population growth and increasing water development costs have prompted many western governments to condition residential development approval on the adequacy of water supplies. We examine the effects of these regulations on housing supply in Colorado and New Mexico using fixed‐effects panel regressions. Our findings suggest that price‐based tools to ensure water availability may be a preferred regulatory alternative to quantity restrictions. Attempts to restrict groundwater basin access have not unambiguously corrected negative externalities related to growth. Meanwhile, Colorado cities' aggressive use of impact fees has facilitated water resource development, without limiting growth. 相似文献