| 泰国的侏罗系 |
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2020-07-24 00:00:00 |
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泰国的侏罗系 本书特色
《泰国的侏罗系(英文)》是第八届国际侏罗系大会地层丛书之一。
泰国的侏罗系 内容简介
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泰国的侏罗系 目录
PREFACEABSTRACTChapter I INTRODUCTIONI. General informationII. Marine Jurassic rocks of ThailandIII. Jurassic LocalityChapter 2 PREVIOUS WORKSChapter 3 REGiONAl GEOLOGIC SETTINGI. Mae Sot-Umphang area, Tak Province, northwestern ThailandII. Phop Phra area, Tak Province, northwestern ThailandIII. Chumphon area, Chumphon Province, Peninsular ThailandIV. Thung Song-Khlong Thom area, Nakhon Si Thammarat and Krabi Provinces, Peninsular ThailandV. Ao Luk-Plai Phraya area, Krabi and Surat Thani Provinces, Peninsular ThailandChapter 4 MARINE JURASSIC ROCKS OF NORTH——WESTERN THAILANDⅠ. Jurassic of the Khun Yuam-Mae Hong Son area1. Lithostratigraphy2. Fauna and age of the Khun Yuam-Mae Hong Son areaⅡ. Marine Jurassic of the Mae Sot area1. Lithostratigraphy2. Fauna and age of the Hua Fai Group in the Mae Sot areaⅢ. Marine Jurassic of the Phop Phra area1. Lithostratigraphy of the Phop Phra area2. Fauna and age of the Phop Phra areaIV. Marine Jurassic of the Umphang area 1. Lithostratigraphy2. Fauna and age of the Umphang areaV. Marine Jurassic of the Kanchanaburi areaChapter 5 MARINE JURASSIC OF PENINSULAR THAILANDI. General InformationII. Marine Jurassic of the Chumphon area1. Lithostratigraphy2. Fauna and age of the Chumphon areaIII. Marine Jurassic of the Nakhon Si Thammarat area1. Lithostratigraphy of the Thung Song-Khlong Thorn area2. Fauna and age of the Thung Song-Khlong Thom areaIV. Marine Jurassic of the Krabi area1. Lithostratigraphy of the Ao Luk-Plai Phraya area2. Fauna and age of the Ao Luk-Plai Phraya areaChapter 6 NON-MARINE JURASSIC OF NORTHERN, NORTHEASTERN,EASTERN AND PENINSULAR THAILANDI. General InformationII. Non-marine Jurassic in the Khorat Plateau, Northeastern ThailandIII. Non-marine Jurassic in northwestern ThailandIV. Non-marine Jurassic in eastern Thailand1. Laem Sing Formation2. Phu Kradung FormationV. Non-marine Jurassic in peninsular Thailand1. Thung Song-Khlong Thom area of Nakhon Si Thammarat and KrabiProvincesChapter 7 FAUNAL ASSOCIATIONS, PALEOECOLOGY AND PALEOENVIRONMENTI. General InformationII. Faunal Associations, Paleoecology and Paleoenvironments1. Bositra Facies2. Benthic Bivalve Facies3. Mixed Facies4. Ammonite Facies5. Brachiopod FaciesChapter 8 MINERAL ASSOCIATIONⅠ. General InformationII. Location, accessibility and topography of the Pha Daeng MineIII. Regional GeologyIV. Pha Daeng and the Surrounding DepositsV. Geology and Mineralization of Pha Daeng Mine1. Geology2. Mineralization3. Genetic Model Chapter 9 DETAILED LITHOSTRATIGRAPHY AND PETROGRAPHY OF THE SELECTEDAREA. IMPLICATIONS FOR DEPOSITIONAL ENVIRONMENT AND TECTONICSⅠ. Detailed lithostratigraphyⅡ. Petrography1. Petrography of the Khun Huai Formation2. Petrography of the Doi Yot Formation3. Petrography of the Pha De FormationⅢ. Sedimentary cycles and sea level change1. Eustatic sea level curves of the Khun Huai Formation2. Eustatic sea level curves of the Doi Yot Formation3. Eustatic sea level curves of the Pha De FormationIV. Depositional environment1. Depositional environment of the Khun Huai Formation2. Depositional environments of the Doi Yot Formation3. Depositional environment of the Pha De FormationV. Tectonic implicationsChapter 10 CONCLUSIONSACKNOWLEDGEMENTSREFERENCES
泰国的侏罗系 节选
《泰国的侏罗系(英文)》内容简介：DuringtheJurassic,Chinaandenvironsasadomainwasborderedbythewesternpalaeo-PacifcineastandbytheTethysinwest,anditwasconnectedtoRussiainnorthandlocatedatthejunctionbetweenthewesternpalaeo-PacificandnortheasternTethys.TheJurassicrocksofChinaandenvironsarethereforethelargestgeologicalbodywhichhasrecordedvariousgeologicaleventshappenedintheTethyan,subborealandpalaeo-Pacificrealmsbothinmarineandnon-marinesystems.
泰国的侏罗系 相关资料
插图：The geology of many regions has been described previously by various workers, e.g. Cotter (1924), Heim and Herschi (1939), Brown et al. (1951), Ward and Bunnag (1964), Sato (1961), Komalarjun and Sato (1964), Sato (1975), Braun and Jordan (1976), Hagen and Kemper (1976), Kemper et al. (1976), Kemper (1976), Chonglakmani (1983), Chonglakmanietal. (1985), Meesooketal. (1985), Charoenpravatetal. (1985), Tantiwanit et al. (1987), Fontaine and Suteethorn (1988), Sato and Westermann (1991), Beauvais and Fontaine (1993), Meesook (1994), Meesook and GrantMackie (1994), Meesook and Grant-Mackie (1996), as follows:The limestone of Ban Yang Puteh, 12 km southeast of the Mae Sot District near a tributary of Huai Mae Ku, was thought to be a continuation of the Kamawkala limestone of eastern Myanmar (Cotter, 1924).During reconnaissance geological surveys in northern Thailand, Heim and Herschi (1939) mentioned the presence of a Late Jurassic-Early Cretaceous formation about 18 km south of Mae Sot District. Some small fossils were found in nodular layers and kidney-shaped concretions of limestone occurring in a "red formation". The nature and details of these fossils were not indicated.Resulting in mineral exploration conducted jointly by geologists of the United States Geological Survey and Thai Department of Mineral Resources, the first geological map of Thailand was published in 1951 on scale of 1 : 2,500,000 (Brown et al., 1951). They also described the general stratigraphy of Thailand and recorded ammonites identified asErycites, Tmetoceras and Ludwigia at Ban Yang Puteh and at a limestone outcrop 3 km to the south-southwest, indicative of early Middle Jurassic age.Hayami (1960) studied the bivalves including Eomiodon chumponensis n sp. in argillaceous sandstone at Haat Sai Ri and Pak Nam Chumphon of Chumphon Province and concluded a probable Jurassic age.
泰国的侏罗系 作者简介
作者：（泰国）米苏克 沙金庚米苏克，A.博士，泰国矿产资源部化石保护局主任，主要从事地层学、古生物学、沉积学研究和矿产资源勘察等。
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