1、geophysical prospecting

geophysical prospecting發(fā)音

英：　　美：

geophysical prospecting中文意思翻譯

常用釋義：地球物理勘探：一種通過(guò)測量地球物理場(chǎng)的變化來(lái)探測地下地質(zhì)結構和礦產(chǎn)資源的科學(xué)方法。

地球物理探測法; 物探

[地質(zhì)]地球物理勘探

geophysical prospecting雙語(yǔ)使用場(chǎng)景

1、Equipment management is of importance in geophysical prospecting.───設備管理在地球物理勘探工作中是非常重要的.

2、Seismic surveying is the most important of the three main types of geophysical prospecting.───地震勘探是三種主要地球物理勘探方法中最重要的一種。

3、Studying seismo electric exploration is a new research in geophysical prospecting.───開(kāi)展震電勘探研究是當今世界地球物理勘探領(lǐng)域一項嶄新的課題.

4、Ni - Cd alkaline rechargeable battery in cylindrical shape is widely used in the geophysical prospecting instruments.───鎘鎳圓柱密封堿性充電電池,被廣泛地使用在物探儀器設備中.

5、Seismic wave velocity is the most important parameter in geophysical prospecting and development.───地震波速度是地球物理勘探和開(kāi)發(fā)中最重要的一個(gè)參數。

6、task of establishing if the sea ever divided Paliki from Kefalonia is about to get easier. Fugro, a geophysical prospecting company, has lent machinery for a full subterranean scan.───海是否曾將帕利克從凱法利尼亞分開(kāi)的任務(wù)變得越來(lái)越容易了，福格洛，一個(gè)地質(zhì)勘探公司，已經(jīng)提供機器來(lái)進(jìn)行地中海的全面掃描，如果地質(zhì)學(xué)家斷定帕利克曾經(jīng)是一個(gè)島，那將進(jìn)一步證明它是古代的愛(ài)塞卡。

7、I was told that the gravitational method is the most inexpensive method among the geophysical prospecting.───我聽(tīng)說(shuō)在所有的地球物理勘探方法中,重力法是最為經(jīng)濟的一種方法.

geophysical prospecting相似詞語(yǔ)短語(yǔ)

1、physical distancing───物理距離

2、geometrical proportion───等比

3、conical projection───[測]圓錐投影；錐形投影

4、conical projections───[測]圓錐投影；錐形投影

5、chemical processing───化學(xué)加工

6、geometrical proportions───幾何比例

7、physical affection───表達親密；肉體之愛(ài)；身體愛(ài)撫

2、Yangyi Geothermal Field in Damxung County（）

Yangyi geothermal field is located 72 km northwest of the Lhasa City，55 km southwest to the Yangbajain geothermal field，50 km from the Nyemo County town，accessible by highways.The altitude ranges 4550-5050 m.

The field lies on the south end of the Yangbajain-Yangyi basin，being a component of the Damxung-Yangbajain-Doqen Co active tectonic belt.The formation and distribution of the field are obviously controlled by the sublati-tudinal and the NE-and NW-trending faults.In the central part of the field there formed the Miocene horst of volcanic rocks，on the east and west sides there is a fault basin overlain by Quaternary argillaceous sandy gravels with a maximum thickness exceeding 600 m on the east side.The cover of the heat reservoir is composed by Himalayan trachyte，volcanic clastics and tuff；under-lain by granite porphyry and granite.High-temperature heat flow exists main-ly in the fractures of granite porphyry and granite，indicating a bedrock-frac-ture type heat reservoir.In plan the Yangyi geothermal field is oval in shape，4 km long from north to south，covering an area of about 1 1 square kilome-ters·The temperature decreases gradually from the center to the periphery.The high-temperature central part has the temperature exceeding 150℃.It covers an area of 1.6 square kilometers，being the major area with rising fluid and also the principal part of the reservoir.The maximum temperature of the reservoir obtained is 207℃.The total amount of steam and water of a single borehole is greater than 100 t/h，the maximum being 381 t/h.The maximum power generation potential of a single hole reaches 10 MWe.Surrounding the high-temperature area lies the medium-temperature geothermal resources area with temperature ranging 90-150℃，covering an area of 5.9 square kilome-ters·The entire field has a relative closing pressure of flowing well ranging 2.8-9.4 kg/cm2，the relative working pressure 0.95-11.3 kg/cm2，the total amount of steam and water of a single well 19-381 t/h，the dryness 13%-26.9%，the inferred accumulative heat at the depth of 2000 m 9.14×1014 kcal，the recoverable heat 5.86×1013 kcal，and the total amount of steam and water exploitable under present conditions 1045 t/h（200℃）；all these demon-strate that the field can satisfy the demands for a 30 MWe geothermal power station with prospective installed capacity of 50 MWe.

There are various kinds of geothermal manifestations in the Yangyi field focused in three NE-trending gullies.Regular geological investigations com-menced in the 1 970s.

In 1974-1975 the Geothermal Group of the Qinghai-Tibet Comprehensive Expedition Team under the CAS observed the hydrothermal activities in the area，and by hydrochemical analysis calculated the natural heat flow to be 2.6×104 kcal/sec.In 1977-1980 Kang Wenhua and others with the Institute of Geomechanics of the CAGS investigated the geological structures and conclud-ed that the heat indications in Yangyi were controlled jointly by the E-W trending Gongbo＇gyamda-Yangbajain fracture in combination with the N-S trending Baingoin-Kangmar fracture.From 1981 to 1984 Liu Lianjie and oth-ers with the Geothermal Geological Party of Tibet made a 1∶100000 geother-mal reconnaissance survey and suggested that the hydrothermal activities wereunder the control of basement fractures.

In 1984-1985 Lei Zixiao，Jing Baofu and others with the Geophysical Prospecting Party of the TBG performed 1∶50000 integrated gravitational，magnetic and electric prospecting there.The area outlined by contours with minimum resistivity less than 10 ohm-m amounted to 4.8 square kilometers，generally identical to the medium-temperature geothermal area，and that out-lined by 15 ohm-m contours was 10.1 square kilometers，roughly identical to the area with temperature exceeding 25℃.

In 1985-1987 detailed survey was conducted in the Yangyi geothermal field by the Geothermal Geological Party of Tibet.The party drilled the first geothermal borehole in June 1985，and evaluated the geothermal resources mainly by drilling.Altogether 19 exploration boreholes were drilled covering a footage of 8087 m，the deepest being 825.5 m；besides，another 13 holes were drilled for temperature-measuring.Also performed were geophysical logging and heat reservoir engineering testing.During this period，the Institute of Geophysical and Geochemical Prospecting with the MGMR carried out soil sur-veys on Hg，As，Sb and Bi；Zhu Meixiang with the Geothermal Office of the Peking University and Li Jiazheng with the China University of Geosciences studied respectively the hydrothermal alteration and the volcanic rocks of the area with favorable results.

In 1 988-1 990 the Geothermal Geological Party explored the field and a to-tal of 1 5 boreholes were drilled at a footage of 11831 m，the deepest being 1149.44 m.In October 1989 when operating the No.208 hole，they obtained a 207℃ heat flow.All boreholes were examined by geophysical logging in coor-dination with heat reservoir engineering testing.In cooperation with Lu Ren and others of the Tianjin Geothermal Prospecting and Exploitation Design In-stitute the party conducted modeling calculation of the heat reservoir and pre-dicted the potential of the field.In 1991 Liang Tingli and others prepared and submitted the“Report on exploration of the Yangyi Geothermal Field”which was examined and approved in December the same year by the State Committee of Mineral Reserves.

Yangyi is so far the highest-temperature geothermal field in China.It is of basement fracture type and has been explored with great difficulty.The Geothermal Geological Party of Tibet and the Geophysical Prospecting Party of the TBG，hand-in-hand with the related research institutions of inland Chi-na，accomplished the prospecting，detailed prospecting and exploration over a period of ten years，and provided the State with an exploitable and utilizable medium-size geothermal field.The heat flow is characterized with high tem-perature，high pressure，large flow amount，and less encrustation，exhibiting a favorable future for the development of the Yangyi geothermal field.