Ⅰ 德國TGE公司簡介
德國TGE公司總部位於德國波恩，是一家在LNG接收站、LNG液化工廠工程設計和項目管理、工程總包服務領域全球領先的企業，而中集是全球第一的LNG儲運裝備生產商。
1、注冊地：盧森堡（Luxembourg）
2、主要辦公地點：43, Route d'Arlon，L-8009 Strassen
3、法定代表人：VLadimir PUKLAVEC
4、公司性質：有限責任公司
5、注冊資本：50,000 EUR
6、主營業務：投資控股
7、主要股東或實際控制人：VLadimir PUKLAVEC
TGE GAS的前身Liquid Gas International Ingenieurgesellschaft GmbH，由私人資本於1981年創立。
1993年，被比利時公司Suez Tractebel SA收購後，更名為Tractebel Gas Engineering GmbH（喬特波氣體工程有限公司），成為Suez Tractebel SA中唯一從事石油化工氣體總承包項目的公司。
2003年，成為Suez Tractebel SA中唯一從事天然氣總承包項目的公司。
2006年，Suez-Tractebel變為TGE Holding GmbH。2007年，TGE Holding GmbH將其離岸業務與在岸業務進行分拆、重組，把有關在岸業務歸入TGE Gas Engineering GmbH，即TGE GAS。
2008年，中集收購了TGE 60%的股份，雙方開始利用各自的資源優勢，共同拓展市場，中集的能化業務得以從單體裝備製造向工程總包服務拓展。
現在TGE的營收已經從收購時的3000萬歐元上升到1億多歐元，提高了四五倍。
TGE GAS是擁有25年經驗的獨立項目總承包商，業務范圍為：在LNG、LPG及其他石油化工氣體的存貯、處理領域，為客戶提供EP+CS（設計、采購和建造監工）等技術工程服務。
主要服務領域包括：大型LNG進出口接收站、中型分銷和衛星站儲存罐區；大型LPG、乙烯、丙烯和液氨等石油化工氣體進出口接收站和儲存罐區；氣體處理工廠等。
TGE GAS有137名員工分別分布在德國波恩、比利時布魯塞爾、英國曼徹斯特、中國上海、台北、斯洛維尼亞，其中，70%為專業技術、業務和管理專家。
(1)southwestgas控股股票價格擴展閱讀：
投資控股公司是指通過持有某一公司一定數量的股份，而對該公司進行控制的公司。投資控股公司按控股方式，分為純粹控股公司和混合控股公司。
投資控股公司具有與兼並活動不同的若干特點：
1.它不需要100%地收購被控企業的股權，甚至不需收購半數股權就能實現有效控制；
2.它不用通告被兼並企業當局和經過艱苦的談判，只是通過購買股票，而通常可以分批購買，因此，實現控制手段最簡單；
3.投資控股公司控制下的各個企業，在法律上都是各自獨立的經濟實體，它們同控股公司在經濟責任上是完全獨立的，相互之間沒有連帶責任。因此，控股公司中各企業的風險責任不會相互轉嫁。
5.由於投資控股公司中各個企業都是獨立的，因此需要各自申報納稅，所以存在雙重納稅的可能。
此外，投資控股公司在組織上也較兼並公司鬆散。
從公司法的角度講，第一我國公司法沒有投資公司的這樣一個概念，在我國公司法中明確規定了只有有限責任公司和股份公司兩種。
所以，單從公司的分類上來說，不存在投資公司這樣的一個類別。
從公司的名稱來講，所謂投資控股公司，一般主要從事經貿、資產、經營類投資范圍，當然主要還要看公司章程中註明的經營范圍。
Ⅱ Oil-Gas Prospecting Models of the Permian Stratigraphic Sequence Framework in the Southwest China
8.11.1Introction
The degree of oil-gas prospecting of marine facies in the Sichuan-Yunnan-Guizhou-Guangxi regionexcept the Sichuan basin has been lower and its progress has also been relatively slower.Especially there has been no example that sequence stratigraphy was applied to oil-gas prospecting.Based on studies of sequence stratigraphy（Chen Hongde et al.and Tian Jingchuan et al.in the issue）,we established Permian oil-gas prospecting models,made the evaluation and prediction of oil-gas and put forward some suggestions.When doing so,we considered the history and present state of the study of this region,controversy focuses and prospecting experiences of similar oil-gas fields abroad（Reymond et al.,1996;Melom et al.,1995;Rosales et al.,1994;Perrodon,1995;Ross,1991;Stephen et al.,1993;Weimer,1994;Jin Yuganet al.,1994）.It should be pointed that all these start only from sedimentology and sequence stratigraphy.More systematic and overall evaluation and selection of prospecting objects will remain to be studied deeper.
8.11.2Hydrocarbon Source Beds
The distribution of hydrocarbon source beds in the sequence framework chiefly has the following characteristics（Table 8.10）.
Table 8.10Hydrocarbon source beds in different genetic types of basins
1）TST contains most of hydrocarbon source beds.It is steadily stratified and widespread.It is large in effective thickness,good in mother material type and high in organic matter abundance.There is a trend that values of such parameters as organic carbon,total hydrocarbon,chloroform,asphalt graally increase from LST to TST,reach peaks to CD,and then decrease to HST（Fig.8.41）.For example,Lower Permian hydrocarbon source beds in the Xichang basin give results below:organic carbon and chloroform asphalts are 0.05%～0.74% and 10～40 ppm for LST sediments,0.85%～1.7% and 200～400 ppm for TST sediments,and 0.24%～0.5% and 40～100 ppm for HST sediments.According to reckoning of oil-generating parameters,the hydrocarbon source beds in TST sediments account for 50%～90% of the total thickness of hydrocarbon source beds in this basin and their oil-gas contents accounts for 80%～100% of the total resource.
Fig.8.41Main hydrocarbon source beds in the sequence framework
1—Ⅰ-type boundary;2—coal measure;3—enriched organic matter level
2）The lower part of HST sediments is an important oil source.It can be seen from Fig.8.41 that the values of the total hydrocarbon,organic carbon and chloroform asphalt there are similar to or even higher than those of TST sediments.Although this part is thinner in thickness,it is widely distributed and high in organic matter content so that it could have large oil-generating potential.
3）The upper part of HST sediments and coal measures in LST sediments are important gas sources.In the central and the west part of the Upper Yangtze region there are as many as 40 beds of coal,of which 5beds are regionally correlatable,occurring in the top of each of Sequences 7～11（Chen Hongde et al.in the issue）and having a total thickness of 50～250 m.Recently,the oil-gas prospecting in the Sichuan basin has shown their important role in the forming and storage of oil-gas.
4）HST sediments of platform basin facies and basin facies are ideal hydrocarbon source beds.In basin sequences hydrocarbon-forming conditions vary with system tracts.The TST was covered mostly by siliceous sediments with a smaller thickness,the LST chiefly by turbidite,and the HST has a large effective thickness,is widespread and is constituted mainly by mudstone,marl and their transitional rocks.It follows that hydrocarbon source beds should mainly be HST sediments.
8.11.3Reservoirs
In the sequence framework there are four groups of favorable reservoir bodies below（Table 8.11）.
1）Reservoir bodies in LST,such as basin bottom fan and slope fan sand bodies,wave-controlled delta sand bodies,incised valley-filling sand bodies,prograded compound sand bodies,debris-mixed turbidite,mound reef complex and alluvial fan sand bodies.
2）Reservoir bodies in TST,such as barrier beach sand bodies,littoral belted sand bodies,river estuary sand bodies,incised valley.filling sand bodies,ne sand bodies,tide-controlled delta sand bodies,shelf shoal sand bodies,redeposited lag grail bodies,reef,mound reef complex,calcareous debris flow sediments,pyroclastic turbidite,fan-delta grail bodies,calcareous debris gravity flow sediments and turbidite fan sand bodies.
3）Reservoir bodies in HST,such as river-controlled delta sand bodies,wave-controlled delta sand bodies,alluvial fan-channel sand bodies,fan-delta grail bodies,calcareous debris gravity flow sediments,turbidite fan sand bodies and dolomite.
4）Sequence boundaries and relevant karst reservoirs,including eluvial lime-dolomitic breccia systems above the sequence boundaries and karst reservoirs below them.
Table 8.11Reservoirs in different genetic types of basins
8.11.4Covers
The distribution of covers in the sequence framework is consistent with that of hydrocarbon source beds（Fig.8.41）and shows the following characteristics:
1）Early TST sediments are the most important covers.This is firstly because the TST usually received the low-velocity deposition of mudstone,marl and silicalite which are compact and homogeneous,rare in grain composition,low in porosity and permeability and hence strong in plug-back capacity.Second,the TST sediments are a landward overlying,retrograded,regional sedimentary body,which is stable and widespread and has a large effective thickness.Third,TST sediments have multiple overlying forms such as toplap,onlap,downlap and sidelap and so cover-closing has different characteristics such as multiple types-underlying,overlying,interbedded,laterally altered and closed-multiple directions,completeness and tightness.Finally,owing to strong plug-back pressure of TST cover sediments,single reservoirs or traps in underlying system tract sediments can be connected to be favorable for forming large-scale united oil-gas pools.
2）Early HST sediments are important covers.
3）River-flood facies,limnetic facies and littoral plain facies in LST and late HST sediments are favorable covers.
8.11.5Traps
Possible types of traps in the sequence framework of this region were established on the basis of the above studies of generation-storage-cover assemblages（Fig.8.42）.
Fig.8.42Possible traps in different sequence frameworks
1.incised valley-filling sand-sequence boundary;2.TST deposited sand body;3.LST turbidite-fault;4.HST gravity flow-fault;5.TST isolated platform-intemal reefs;6.TST reef-beach complex;7.isolated platform-marginal reefs;8.isolated platform-marginal beach-reef complex;9.HST calcareous debris flow sediment;10.HST channel sand body;11.HST delta sand body;12.old karst;13.TST reefs-fault;14.HST debris flow sediment;15.TST turbidity fan sediment;16.HST turbidity fan sediment;17.carbonate isolated platform facies' thinning out;18.bioclastic beach facies' thinning out;19.littoral belted sand body
In the sequence framework of the Upper Yangtze craton gentle slope,possible traps and their features areas follows:
1）HST sediments enclose carbonate builps in onlap and underlap mudstone;
2）HST isolated carbonate builps or riffles developed in offshore highlands are covered by TST and HST marls;
3）HST internal gentle slope skeletal fragment beach sand bodies thin out seawards in offshore compact wackestone;
4）Ⅰ-type boundaries and internal gentle slope sediments below them were karsted;
5）Inclined internal gentle slope sediments were truncated at regional unconformities;
6）LST sediments separated from early HST internal gentle slope sediments were onlapped and underlapped by external gentle or basin mudstone;
7）Grain lime-dolomite is separated by shoreline facies sediments;
8）Single carbonate grain rock riffles,tidal bar,tidal channels or patch reefs are lonely located in gentle slope wackestone;
9）Internal gentle slope grain limestone dips up and thinned out in compact internal gentle slope wackestone.
In the sequence framework of the Upper Yangtze craton platform,possible traps and their features are as follows:
1）Incised valley-filling sand bodies and sequence boundaries were truncated by overlying TST sediments;
2）Early TST modified and redeposited sand bodies are enclosed by TST sediments;
3）LST turbidite was overlaid by TST sediments;
4）HST calcareous debris gravity flow sediments thinned out platformwards and basinwards and were enclosed by basin facies siliceous marl and TST marlite;
5）Grain limestone（or lime-dolomite）was enclosed by contemporaneous low energy sediments;
6）HST reef knolls were enclosed by other contemporaneous sediments and TST sediments;
7）TST estuary sand bodies were overlaid by contemporaneous silty mudstone;
8）LST wave-controlled delta sand bodies were overlaid by TST silty mudstone;
9）TST tide-controlled delta sand bodies were overlaid by contemporaneous silty mudstone;
10）HST river-controlled delta sand bodies were overlaid by contemporaneous mudstone;
11）Sequence boundaries were karsted;
12）TST reef knoll-limestone rises were enclosed and covered by contemporaneous sediments;
13）LST reef knoll-limestone was overlaid and closed by TST sediments;
14）TST littoral belted sand bodies and barrier beach sand bodies were enclosed and covered by contemporaneous sediments;
15）TST calcareous debris flow sediments were enclosed and covered by contemporaneous sediments.
In the sequence framework of the Youjiang rift basin,possible traps and their features are as follows:
1）Isolated carbonate platforms were enclosed and covered by platform basin facies;
2）LST turbidite was enclosed by TST sediments;
3）TST pyroclastic turbidite was encircled by contemporaneous basin facies;
4）HST calcareous debris gravity flow sediments were overlaid and truncated by basin facies and TST sediments;
5）HST back-reef-dolomite was overlaid and truncated by TST limestone;
6）TST mound-beach-reef-limestone was onlapped by CD at the top of the TST sediments;
7）LST mound-reef-limestone was enclosed by TST sediments;
8）Old karst existed.
In the sequence framework of the Shiwandashan foreland basin,possible traps and their features are as follows:
1）LST basin bottom fan sand bodies were overlaid by TST sediments of a very large thickness and the vertical and lateral closing of covers is not good;
2）TST fan delta grail bodies were overlaid by HST sediments and are rich in oil and gas,but their closing and storage conditions are not good;
3）HST fan delta front sand bodies were overlaid by fan delta plain and alluvial fan plain sediments and have better cover conditions;
4）LST alluvial fan grail bodies were enclosed by contemporaneous sediments and are not good in generating and covering conditions;
5）HST alluvial fan sand bodies were overlaid by TST sediments;
6）TST turbidity fan grail bodies were enclosed and covered by contemporaneous sediments.
In the sequence framework of the Qinzhou-Haifang passive margin strike-slip basin,possible traps and their features are as follows:
1）LST calcareous debris turbidite was overlaid by TST sediments;
2）TST calcareous debris flow sediments were enclosed and covered by contemporaneous sediments；
3）HST caocareous debris gravity flow sediments thinned out basinwards and platformwards and wer eoverlaid by TST sediments；
4）Carbonate isolated platforms were enclosed and covered by basin facies;
5）Overlap unconformabilities existed on the slope of the NW side of the basin;
6）Hidden reefs are located on the NW side of the basin;
7）Old buried hills are located in the middle uplift belt of the basin;
8）Early Permian carbonate rocks and their top karst reservoirs were overlaid by Late Permian foreland basin sediments of a very large thickness.
8.11.6Prospecting Suggestions
On the basis of the above analyses,it can be concluded that①every system tract is a relatively independent oil-forming system,which is constituted by many possible non-tectonic traps or forming-storage associations；②every system tract is largely and oil-gas prospecting system,which consists of many small oil reservoirs and gas pools;and③compared with those in classic rocks,the trap and distribution of oil and gasin carbonate rocks are heterogeneous,hidden and complicated.
There are six large-scale depression areas in the Sichuan.Yunnan-Guizhou-Guangxi region:the Sichuan basin,the Shiwandashan basin,the Nanpanjiang depression,the Xichang basin,the South Guizhou depression and the Central Guangxi depression.In order to select objects of oil-gas prospecting,we made comparisons among these six depression areas.Our suggestions are as follows:
1）In respect of target beds which should be selected,the first is old karst intervals controlled by Ⅰ-type sequence boundaries（the top of the Maokou Formation,the top of Pre-Permian,the top of the Changxing Formation and the top of Sequence 5）,the second is mound-beach-reef-dolomite and calcareous debris gravity flow sediments in the upper part of HST related to Ⅱ－type sequence boundaries（as in the Changxing Formation and the Maokou Formation）,and the third is HST mound-reef-limestone and LST turbidite（as in the Changxing Formation and the Maokou Formation）.
2）In respect of target areas which should be selected,the first is the Sichuan basin,the second the Shiwandashan basin,the third the Nanpanjiang depression and the Xichang basin,the fourth the South Guizhou depression and the final the Central Guangxi depression.
3）Possible traps or oil-gas pools which prospecting efforts should be concentrated on are as follows:
The Shiwandashan basin:karst traps,onlap unconformability traps,hidden reef traps and calcareous debris gravity flow traps in the northwestern side;old hidden hill traps in the central;and fan delta traps and turbidity fan traps in the southeastern part.
The Nanpanjiang depression:carbonate isolated platform traps,hidden reef traps and hidden gravity flow sediment traps.
The Xichang basin:old karst traps,delta traps,onlap unconformability traps and hidden mound-reef traps.
The South Guizhou depression:hidden reef traps,gravity flow sediment traps and onlap unconformability traps and others.
The Central Guangxi depression:hidden reef-beach traps,carbonate isolated platform traps,old karst traps and so on.