再论东河砂岩孔隙成因──以塔中地区为例
- 塔里木石油勘探开发指挥部勘探开发研究院,新疆库尔勒 841000
作者简介:
孙玉善，男，1954年出生，工程师，石油地质。
- 收稿日期:
1999-04-01
- 修回日期:
1999-05-17
- 刊出日期:
1999-12-10
摘要: 塔里木盆地并下东河砂岩埋藏深、储层优质，属国内外罕见，对其成因众说纷法。本文依据岩石学特征，针对不同类型的孔隙演化特征与其物性参数，对孔隙的成困类型进行分析后认为：东河砂岩储集空间类型主要以压实剩余的原生粒间孔为主，在部分压实或半充填的剩余（残留）粒间孔隙背景中发育有以溶蚀石英及铝硅酸盐等，而微度扩大的次生和原生混合型孔隙。原生粒间孔隙保存的条件与多种地质因素联合、复合作用关系极为密切。
Rediscussion on Pore Genesis of Donghe Ssndstone——An example from Tazhong area
- Tarim Petroleum Exploration and Development Headquarters, Karla, Xinjiang, 841000
- Received Date:
1999-04-01
- Rev Recd Date:
1999-05-17
- Publish Date:
1999-12-10
Abstract: Donghe sandstone is typical shore-shallow-sea facies quartz sandstone with burial depth ranging from 3500 to 5100m and the largest thickness 129 meter formed during late Devonian (or early Carboniferous) in Tarim basin. Although it has great depth, it still has better reserroir quality (Porosity is about 20% and permeability 200 ×10-3μm2 ) and that is quite rare in the world. Different vie wpoints on its genesis yet exist.Some believe that the well-developped porosity was formed by dissolwtion of calcite cement in late diagenesis,but the others think it is primary proe retained after compaction and cementation. On the basis of mrmeraus data collected from casting section,thin section and SEM,the anthor draw a conclusion that pare in Dongre sandstone is chiefly primary porosity retained. after compaction and cementation; and the proofs are as follows:First,tire cornpaciion intensity on porasity is not strong and pore fillings come mainly from autirigenic clay,quartz and calcite nriner}als ilr wtrich tire clayfilm is the most common infillins form,and next clay fill,quartz overgrowth as well as carbonate fill. The carbonate cement is abundantly distributed around the sardbody, but irl the middle they present in spot,grutneleuse and laminae. Second dissolotion is raot well developped in the sandstone snd they mainly take place in class, quartz overgrowth and quartz grain us vela as feldspars while the carboncate cereut shows no any dissolution and they are not the remains produced by intersive dissaieaion. Under the background of the remained intergranular pore,the mixed pares formed by the remained primary pore and the secondary dissalution pore. Dissolution has the eminent contribution to the sandstone permeability. By quantitative analysis on tire evolution of porosity and related physical property parametevs,the author believe that the primary pore. suchas the pare with well-developped clove film and substrate loss porosity 17.82% by canpaction,and the other forms of loss by filling and compaction is 20%,27 % and 34.3%, respectively. The secondary dissalution can increase part of porosity by 1.49%. The protection condition of primary porasity has close relatian to the intgerated gealagicalfactors.
孙玉善, 杨帆. 再论东河砂岩孔隙成因──以塔中地区为例[J]. 沉积学报, 1999, 17(S1): 699-705.
| 引用本文: |
孙玉善, 杨帆. 再论东河砂岩孔隙成因──以塔中地区为例[J]. 沉积学报, 1999, 17(S1): 699-705.
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SHUN Yu-shan, YANG Fan. Rediscussion on Pore Genesis of Donghe Ssndstone——An example from Tazhong area[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 699-705.
| Citation: |
SHUN Yu-shan, YANG Fan. Rediscussion on Pore Genesis of Donghe Ssndstone——An example from Tazhong area[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 699-705.
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