泰国湾西部表层沉积物重矿物分布特征:对物质来源和沉积环境的指示

对泰国湾西部159个表层沉积物进行了碎屑重矿物鉴定分析,其中57站重矿物颗粒数少于300粒,有效数据102站。结果表明,泰国湾西部表层沉积物中重矿物含量低,平均为1.628%,变化范围在0.016%~20.755%之间;共鉴定出重矿物29种,包括菱铁矿、褐铁矿、普通角闪石、自生黄铁矿、赤铁矿、绿帘石、磁铁矿、白钛石、锆石、紫苏辉石、石榴子石、黑云母、水黑云母、普通辉石、透闪石、白云母、钛铁矿、白云石、榍石、磷灰石、绢云母、蓝晶石、十字石、阳起石、电气石、金红石、棕闪石、独居石和透辉石,其中优势矿物为菱铁矿、普通角闪石和褐铁矿,平均含量(颗粒百分含量,下同)分别为41.6%,15.6%和13.4%,最高含量分别为99.7%,72%和94%;特征矿物为自生黄铁矿、磁铁矿、赤铁矿和锆石,平均含量分别为6.8%,4.1%,3.9%和0.9%,最高含量分别为97.3%,26.0%,91.7%和11.0%。利用数学聚类方法并结合矿物分布,在泰国湾西部划分出6个重矿物分区,基本以从北到南垂直岸线的东西向带状分布,矿物分区与物质来源和沉积环境具有较好的对应关系。重矿物来源主要为陆源和自生源:前者以普通角闪石、磁铁矿、赤铁矿、钛铁矿以及紫苏辉石等为代表性矿物,陆源物质输入较为明显的海区有3处,即曼谷湾的罗勇外部海区、春蓬和敦沙之间的近岸区域以及宋卡和北大年之间近岸区域,其中春蓬和敦沙之间的近岸区域表层沉积物中黑色金属矿物含量高,与附近有铁矿床分布相符合;后者以菱铁矿、自生黄铁矿以及菱铁矿风化形成的褐铁矿为代表性矿物,主要分布在陆架中南部、中东部和中北部。依据自生源矿物分布特征在陆架中部划分出不同的沉积环境,在陆架中南部和中北部为轻度还原环境,局部出现较强的还原环境,而在陆架中南部的轻度还原区域内出现氧化沉积环境。     

真美呀! 泰王国的湄南河

东南亚最大的河流之一泰国的第一大河泰国河流中水量最大的河湄南河(Menam River),在泰国又叫昭披耶河,东南亚最大的河流之一。发源于泰国北部山地,流到南部平坦地区,形成湄南河三角洲     

南海西南部巽他陆架底层冷水及其季节变化分析

本文利用历史水文观测数据研究了南海西南部巽他陆架水团特征,结果表明:(1)巽他陆架纳土纳群岛周围底层存在着低温高盐的冷水,该冷水沿地形爬升分为两支,一支可延伸至泰国湾,另一支伸向卡里马塔海峡;(2)巽他陆架底层冷水有明显的季节变化,该底层冷水在春季开始形成,夏季达到最强,秋季开始衰退,最后在冬季完全消失;(3)巽他陆架底层冷水来源于南海次表层水的涌升。夏季西南季风使陆架表层水向南海流动,有利于南海次表层低温高盐水沿地形向陆架爬升,此时底层冷水与表层水温差超过8°C。冬季东北季风,使南海表层水向陆架流动,海水在陆架堆积,从而阻止了南海次表层低温高盐水的爬升。     

泰国西部比洛克（Pilok）锡钨矿区二长花岗岩SHRIMP 锆石U-Pb 年龄及其地质意义

使用SHRIMP 技术测得泰国西部比洛克（Pilok）钨锡矿区的2 件二长花岗岩的锆石U-Pb 年龄分别为181.7±4.8Ma和175.3±3.3Ma,属于早侏罗世Toarcian 期,代表了岩体的侵位年龄。岩石主量和微量元素特征分析表明,比洛克钨锡矿区的二长花岗岩为高钾钙碱性S 型过铝质花岗岩。结合区域地质特征,比洛克矿区二长花岗岩应是班公湖—怒江—抹谷洋壳向西侧的腾冲—德林达依陆块俯冲的产物。     

赴泰国访问有感——记参加世界气象组织第七届人工影响天气科学讨论会

遵照中国气象局的指示,我们作为中国气象局人工影响天气代表团一行１３人,于１９９９年２月１６日从广州出发,去泰国参加世界气象组织第七届人工影响天气科学研讨会。我们经曼谷于当天晚上到达清迈。一下飞机扑面而来的是一股湿热的空气,还挟带着一股热带植物的草木花...     

山东亚特尔集团向泰国出口设备

近日,山东亚特尔集团向泰国某公司出口两台4R雷蒙机。继打开越南市场后,集团在东南亚地区又成功开拓了泰国市场,为下步占据东南亚市场奠定了坚实基础。     

Ecohydrology from Concepts to On-ground Actions： Report of Special Side Event on Ecohydrology--An Interdisciplinary Challenge, January 5-7, 2009 in Bangkok, Thailand

International Hydrological Programme Ⅶ (IHP-Ⅶ) directs the research objectives of hydrologists all over the world from 2008 to 2013. As a key programme contributed to the IHP Ⅶ, UNESCO's Ecohydrology Programme (EHP) has evolved into a trans-disciplinary scientific programme to analyze dynamic relationships between hydrological, social and ecological systems. Twenty international experts from 12 countries were invited by UNESCO to attend the side event on "Ecohydrology--An Interdisciplinary Challenge" in Bangkok, Thailand. It aimed to synthesize knowledge gaps for addressing issues related to critical water systems. This event focused on how better knowledge of the interrelationships between the hydrological cycle, livelihoods and ecosystems could be contributed to more cost-effective and environmental-friendly management. The five themes of the event with 20 keynote lectures were given as fellows.     

Study on the geochemical characteristics of ocean-ridge and oceanic-island volcanic rocks in the Nan-Uttaradit zone,northern Thailand

Field investigations and laboratory integrated research as indicated that ophiolite mélange in the Nan-Uttaradit zone, northern Thailand, consists of fragments of tectonites such as metamorphic peridotite (extremely silicified serpentinite), cumulates (pyroxenolite, gabbro, and gabbro-diorite), ocean-ridge basalt, oceanic-island ba-salt and radiolarian silicalite, and it was formed during D3-P. The rock series, rock types and petrogeochemical characteristics of metamorphic tholeiites in the Nan area of the Nan-Uttaradit zone are similar to those of ocean-ridge basalts (C1) in China's Ailaoshan zone. As for the Hawaiites in the Nan area of the Nan-Uttaradit zone, their major elements, REEs and trace elements are similar to those of oceanic-island basalts in China's Jinshanjiang zone (P11). In the Uttaradit area of this zone the metamorphic alkaline basalts show transitional petrogeochemical characteristics between ocean-ridge basalts and oceanic-island basalts, which were still formed in oceanic-island environments. The above-described basalts are all oceanic volcanic rocks and they are the most important part of the Paleo-Tethys oceanic crust in the Nan-Uttaradit zone.