Please use this identifier to cite or link to this item:
http://nopr.niscpr.res.in/handle/123456789/42979Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Li, Ying | - |
| dc.contributor.author | Xu, Shouyu | - |
| dc.date.accessioned | 2017-10-30T06:27:12Z | - |
| dc.date.available | 2017-10-30T06:27:12Z | - |
| dc.date.issued | 2017-11 | - |
| dc.identifier.issn | 0975-1033 (Online); 0379-5136 (Print) | - |
| dc.identifier.uri | http://nopr.niscair.res.in/handle/123456789/42979 | - |
| dc.description | 2191-2200 | en_US |
| dc.description.abstract | Different carbonate types found in Tahe Oilfield and their petrological characteristics are analyzed. Primary rock types include sandy limestone, bamboo-like limestone, sandy limestone, dolomitic micrite, particle limestone, limestone containing organic matter, micrite, and siliceous fine crystalline dolomite containing calcite, in which cracks or fissures are mainly or locally developed. The main reservoir space types are also studied. Intergranular or intragranular dissolved pores constitute the main pore types in the study area, with intergranular holes and intergranular dissolved pores playing a secondary role. | en_US |
| dc.language.iso | en_US | en_US |
| dc.publisher | NISCAIR-CSIR, India | en_US |
| dc.rights | CC Attribution-Noncommercial-No Derivative Works 2.5 India | en_US |
| dc.source | IJMS Vol.46(11) [November 2017] | en_US |
| dc.subject | Tahe Oilfield | en_US |
| dc.subject | Carbonate reservoir | en_US |
| dc.subject | Fractured-vuggy system | en_US |
| dc.title | Reservoir fracture cave characteristics of middle - lower Ordovician carbonate rocks in Tahe oilfield in Tarim Basin, China | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJMS Vol.46(11) [November 2017] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJMS 46(11) 2191-2200.pdf | 1.22 MB | Adobe PDF | View/Open |
Items in NOPR are protected by copyright, with all rights reserved, unless otherwise indicated.