四川盆地,Sichuan Basin
1)Sichuan Basin四川盆地
1.Formation and conservation mechanism of the high-quality reservoirs in Sinian-lower Palaeozoic inSichuan Basin;四川盆地震旦系—下古生界优质储层形成与保存机理
2.Study on fluid inclusion of tight sand reservoir of Upper Triassic Xujiahe Formation in centralSichuan Basin;四川盆地中部须家河组致密砂岩储层流体包裹体研究
3.Changxing Formation biohermal gas pools and natural gas exploration,Sichuan Basin;四川盆地长兴组生物礁气藏及天然气勘探
英文短句/例句
1.Contrast analysis of geological conditions between central and west Chuxiong basin and Sichuan basin楚雄盆地与四川盆地中西部地质条件对比分析
2.Regionalization of Mesozoic-Cenozoic Strata and Basin-Range Evolution along the West Margin of Sichuan Basin四川盆地西缘中新生代地层区划及盆山演化
3.Study on the Carboniferous Palaeokarst Landform in Eastern Sichuan Basin四川盆地东部黄龙组古岩溶地貌研究
4.Study on the Law of Formation of the Reservoirs in Caledonian Palaeohigh四川盆地加里东古隆起成藏规律研究
5.Some New Knowledge of Caledonian Paleo-uplift in Sichuan Basin对四川盆地加里东期古隆起的新认识
6.A Forward and Inversion Study on the Main Density Interfaces in Sichuan Basin;四川盆地主要密度界面正、反演研究
7.A Preliminary Study on the Techniques of Producing Porcelain in Tang and Song Dynasties in Sichuan Basin;四川盆地唐宋时期制瓷工艺初步研究
8.GAS SUPPLY-DEMAND PREDICTION AND MARKET PROSPECT IN SICHUAN BASIN;四川盆地天然气供求预测和市场展望
9.PROSPECTS FOR DEVELOPING NATURAL GAS IN SICHUAN BASIN IN THE EARLY PART OF THE 21ST CENTURY;21世纪初叶四川盆地天然气发展前景
10.An analysis of natural gas marketing -Case study: Sichuan basin天然气营销战略分析——以四川盆地为例
11.Stereoscopic exploration new progress of natural gas in Sichuan Basin四川盆地天然气“立体勘探”新进展
12.Reservoir characteristics of the Upper Triassic Xujiahe Formation in Sichuan Basin,China四川盆地上三叠统须家河组储集特征
13.Western Sichuan Depression is a foreland basin developed in the west of Sichuan basin since late Triassic.川西坳陷是指四川盆地西部晚三叠世以来形成的前陆盆地。
14.Study on Field Seismic Acquisition Methods in Zhenba Mountainous Region, Sichuan Basin;四川盆地镇巴山地地震勘探野外采集方法研究
15.The Sequence Stratigraphics Characteristics of Upper Permian in the Northeastern Sichuan Basin四川盆地东北地区上二叠统层序地层特征研究
16.SALTNESS AND GEOLOGIC BACKGROUND OF THE CAMBRIAN STRATA IN THE SICHUAN BASIN IN THE UPPER YANGTZE AREA上扬子区(四川盆地)寒武系的含盐性与地质背景
17.Characteristics of Geological Structure and predication of Gas Prospect of Sichuan Basin四川盆地地质构造特征及天然气远景预测
18.Resource Advantages of the Underground Brines of Sichuan Basin and the Outlook of Their Comprehensive Exploitation四川盆地地下卤水资源优势及综合开发前景
相关短句/例句
the Sichuan Basin四川盆地
1.Regional Dense Fog Time Sequence with Its Annual and Decadal Variation inthe Sichuan Basin;四川盆地区域性浓雾序列及其年际和年代际变化
2.Characteristic of the Flora in the Zhenzhuchong Formation and the Jurassic-Triassic Boundary inthe Sichuan Basin四川盆地珍珠冲组植物群特点及侏罗系与三叠系界线的厘定
3.The sandstone reservoir of Xujiahe Formation in the Western Depression ofthe Sichuan Basin,is the main gas producing zone of the West Sichuan district.四川盆地西部坳陷须家河组砂岩储层是川西地区主要产气层段,该储层孔隙度、渗透率极低,裂缝是储层的主要渗滤通道,裂缝对储层含气性起重要作用,裂缝特征识别及分布在储层评价中较关键。
3)east Sichuan basin四川盆地东
1.The karst rocks in the Carboniferous Huanglong formation is one of the major gas reservoir types in the area between the northern Chongqing and Linshui ineast Sichuan basin.石炭系黄龙组岩溶岩是四川盆地东部渝北—邻水地区天然气藏最重要的储层之一,依据其结构特征,将该岩溶岩系划分为弱溶蚀岩溶岩、中等溶蚀多孔状岩溶岩、强溶蚀角砾状岩溶岩和强溶蚀交代次生灰质岩溶岩等4种类型,以及淡水方解石和白云石2种胶结物类型。
4)Sichuan Basin region(SCBR)四川盆地地区
1.The Sichuan and adjacent areas is divided into southwest China region(SWCR)and Sichuan Basin region(SCBR)according to tectonic backgrounds and seismic damage distribution features.根据地震构造环境和震害分布特点,将四川及邻区划分为西南地区和四川盆地地区。
5)southwest Sichuan Basin四川盆地西南部
6)northwestern Sichuan Basin四川盆地西北部
1.Study on reservoir of the Leikoupo Formation of Middle Triassic innorthwestern Sichuan Basin;四川盆地西北部中三叠统雷口坡组储层研究
2.Sedimentary facies and palaeogeography ofnorthwestern Sichuan Basin during the Leikoupoan(Middle Triassic);四川盆地西北部中三叠世雷口坡期岩相古地理
延伸阅读
四川盆地四川盆地位于中国四川省东部。中国著名红层盆地,中国各大盆地中形态最典型的盆地。面积约20万平方千米。长江把它和东海一脉相连,是中国最大的外流盆地。盆地地势由西北向东南倾斜,海拔一般在250~750米,盆地最高点海拔1800米,为华蓥山脉的最高峰。盆地四周多为海拔1500~3000米的山脉和高原。东有巫山、南有大娄山,西是川西高原、邛崃山及龙门山,北面是秦岭、大巴山。盆地内部有大面积丘陵和低山分布,其中丘陵约占盆地面积52%,为典型的丘陵性盆地。盆地岩性简单。主要由三叠纪长英砂岩、侏罗、白垩纪红色(或紫色)砂页岩及泥岩,第四纪松散堆积物组成。又被称为红色盆地或紫色盆地。长江横贯本区南部,盆地内河流均汇入长江,形成不对称向心状水系。长江北岸的主要支流从西至东有岷江、沱江、嘉陵江及其支流涪江、渠江、大宁河等;南岸主要有长宁河、永宁河、赤水河及乌江等。根据岩性,构造和地貌形态的不同,在盆地内可划分为3个地貌区:东部平行岭谷区,由大小20余条北东向平行褶皱背斜山岭组成,海拔700~1000米;中部方山丘陵区,海拔多在700米以下;西部平原区,平均海拔500~600米。属亚热带湿润季风气候。冬暖夏热,冬季极端最低气温一般大于-5℃,极端最高气温大于40℃,7月均温多高于26℃,长江及其支流谷地可高达28~30℃,为中国著名的高温中心之一。盆地无霜期290~350天,长江河谷全年均为生长季。湿度大,年平均相对湿度和各月平均相对湿度均为70%~80%,年际、月际变化很小。年均云量7.5~8.0。盆地多雾,日照少,年平均日照时数只有1300小时,仅为全年可照时数的20%~30%,是中国日照时数最少地区。盆地中土壤疏松、肥沃,灌溉便利,农业发达。产水稻、小麦、玉米、棉花、甘蔗、蚕丝、茶叶、油菜、药材和水果。有煤、铁、盐、天然气和石油等矿藏。