SUN Haofei,born in 1989,MSc.,engineer,is engaged in petroleum and natural gas geological research and exploration deployment. E-mail: sunhaofei@petroChina.com.cn.
Mianyang-Guang'an Trough in Sichuan Basin is an intra-platform depression developed within the Upper Yangtze Platform during the Late Permian to Early Triassic. This trough,with a water depth between fair-weather wave base and maximum storm wave base,transitions northward into slope facies. In Mianyang-Guang'an Trough,the Changxing Formation,deposited during the Late Permian,is characterized by numerous patch reefs/shoals with minimal dolomitization. By integrating petrographic analysis with Integrated Nonstationary Process Empirical Function Analysis(INPEFA),the Changxing Formation can be subdivided,in an ascending order,into the 1st Member(SQ1-HST and SQ2-TST),lower part in the 2nd Member(SQ2-HST),middle part in the 2nd Member(SQ3),and upper part in the 2nd Member(SQ4). The 1st Member is mainly composed of micritic limestones intercalated with shales and mudstones,which constructed a ramp. The 2nd Member,in contrast,is characterized by grainstones and framestones,which formed a rimmed platform. Mianyang-Guang'an Trough,which developed during the deposition of the 2nd Member,comprises four subfacies,including shoals,reefs,inter-shoal zones and off-reef seafloor deposits. The shoals,which are commonly associated with HST in SQ2,SQ3 and SQ4,are mainly formed by skeletal grainstones,and characterized by low GR(29.3~34.6 API)and relatively low CNL values(13.3%~18.0%). The reefs,developed in the SQ4-TST,are formed of framestones and/or dolomitic framestones,and characterized by relatively low GR(34.0~37.3 API),and relatively high CNL values(19.0%~22.0%). The inter-shoal zones,developed in both HST and TST,consist of wackestones and packstones that are characterized by low CNL(9.9%~11.3%),low RT(33.1~37.3 Ω·m), low DEN(2.55~2.57 g/cm3),and low GR values(26.0~29.5 API). The off-reef seafloor deposits,which consist of intercalated micritic limestones,siltstones and mudstones,are commonly associated with the SQ2-HST,and characterized by serrated log curves. In terms of petrographic and stratigraphic characteristics,reefs and shoals developed in Mianyang-Guang'an Trough are comparable to those in the platform-interior facies,but distinct from those in the platform margins. The stratigraphic and sedimentary characteristics of the Changxing Formation in Mianyang-Guang'an Trough can provide a novel geological model for deciphering trough facies on the carbonate platforms,but also offer theoretical support for exploration in this region.
| 科 Family | 属数 Number of genus | 种数 Number of species | 占总种数比例 Percentage of total species (%) | 属 Genus | 种数 Number of species | 占总种数比例 Percentage of total species (%) |
|---|---|---|---|---|---|---|
| 鹅膏菌科Amanitaceae | 2 | 11 | 5.26 | 鹅膏菌属 Amanita | 10 | 4.78 |
| 小菇科 Mycenaceae | 2 | 12 | 5.74 | 丝盖伞属 Inocybe | 5 | 2.39 |
| 多孔菌科 Polyporaceae | 8 | 14 | 6.70 | 蜡蘑属 Laccaria | 5 | 2.39 |
| 红菇科 Russulaceae | 3 | 23 | 11.00 | 小皮伞属 Marasmius | 6 | 2.87 |
| 小菇属 Mycena | 11 | 5.26 | ||||
| 光柄菇属 Pluteus | 5 | 2.39 | ||||
| 红菇属 Russula | 17 | 8.13 | ||||
| 栓菌属 Trametes | 5 | 2.39 |