A New Juvenile Specimen of Lufengosaurus Huenei Young, 1941 (Dinosauria: Prosauropoda) from the Lower Jurassic Lower Lufeng Formation of Yunnan, Southwest China

A skull and a series of associated cervical vertebrae （ZLJ0112） discovered from the Lower Lufeng Formation （Lower Jurassic） are determined as a juvenile specimen of Lufengosaurus huenei Young 1941 based on amended autapomorphies. Differences between ZLJ0112 and the holotype （subadult specimen） are considered as ontogenetic characteristic changes of L. huenei. Since some of these differences are present in other prosauropod dinosaurs （i.e., forms of the maxillary vascular foramen are irregular; the frontal contribution to the dorsal margin of the orbit is substantial; the frontal contribution to the supratemporal fossa is absent; the supratemporal fenestra is visible in lateral view; the supraoccipital inclined at 75 degrees; the parasphenoid rostrum lies level with the occipital condyle; the retroarticular process is short; the axial postzygapophysis project caudally beyond the end of the centrum） they may be common ontogenetic changes in prosauropod dinosaurs.

A New Theropod Dinosaur from the Middle Jurassic of Lufeng,Yunnan,China

A new theropod dinosaur, Shidaisaurusjinae gen. et sp. nov., has been described on the basis of an incomplete skeleton. The specimen was found near the base of the Upper Lufeng Formation （early Middle Jurassic） in Yunnan, China. It is the first theropod dinosaur from the Middle Jurassic of Yunnan. Shidaisaurus jinae is distinguishable from other Jurassic theropods by certain features from the braincase, axis, and pelvic girdle. The absence of any pleurocoels in the axis or in any anterior dorsal vertebrae suggests that the new Lufeng theropod is relatively primitive and more plesiomorphic than most of the Middle to Late Jurassic theropods from China. Most Chinese taxa of Jurassic theropod dinosaurs have not been well described; a further detailed study will be necessary for us to determine their phylogenetic relationships with Shidaisaurusjinae.

The Late Early Cretaceous Mo Mineralization in the South China Mo Province: Constraints from U–Pb and Re–Os Geochronology of the Lufeng Porphyry Mo Deposit

Compared to other Mo provinces,few studies focused on the South China Mo Province(SCMP),especially for Early Cretaceous Mo mineralization.The Lufeng porphyry Mo deposit in the SCMP is characterized by disseminated and veinlet-type mineralization in granite porphyry,gneiss,and rhyolite.In this study,six molybdenite samples yield a Re–Os isochron age of 108.0±1.8 Ma,which is consistent with the zircon U–Pb age of the granite porphyry(108.4±0.8 Ma).The coincidence of magmatic and hydrothermal activities indicates that Mo mineralization was associated with the intrusion of granite porphyry during the late Early Cretaceous.A compilation of U–Pb and Re–Os chronological data suggests that an extensive and intensive Mo mineralization event occurred in the SCMP during the late Early Cretaceous.The marked difference in molybdenite Re contents between Cu-bearing(85–536 ppm)and Cu-barren(1.3–59 ppm)Mo deposits of the late Early Cretaceous indicates that the ore-forming materials were derived from strong crust–mantle interactions.Together with regional petrological and geochemical data,this study suggests that late Early Cretaceous Mo mineralization in the SCMP occurred in an extensional setting associated with the roll-back of the Paleo-Pacific slab.

Miocene paleoenvironmental evolution based on benthic foraminiferal assemblages in the Lufeng Sag, northern South China Sea

The Miocene epoch marks the most crucial period during the Cenozoic cooling trend, characterized by the Middle Miocene Climatic Optimum(MMCO) and a series of short–lived cooling events(Miocene isotope events).To understand the paleoenvironmental evolution along the shallow water shelf in the South China Sea during the Miocene, the benthic foraminiferal assemblage and total organic carbon content(TOC) were analyzed at Hole LF14 located in the Lufeng Sag, northern South China Sea. Three benthic foraminiferal assemblages(e.g., the Uvigerina spp. assemblage, the Cibicides spp. assemblage, and the Cibicidoides spp. assemblage), corresponding to different watermass conditions, were recognized based on Q–mode factor analysis. Early studies suggested that Hole LF14 was deposited under semienclosed bay, middle to outer shelf or even upper bathyal environment during ～18.7–4.53 Ma. The dominant Uvigerina spp. assemblage was characterized by low diversity and shallow infaunal to infaunal species, indicating a warm, low–oxygenation and eutrophic conditions since the Early Miocene to MMCO(～18.7–14.24 Ma). An abrupt sea level drop and significant faunal changes were recorded during 14.24–13.41 Ma, suggesting development of the East Antarctic Ice Sheets, which resulted in a drop of sea level and change in benthic foraminiferal assemblages along the shallow water shelf. Beyond the Uvigerina spp.assemblage, the Cibicides spp. assemblage became important during the middle–late Middle Miocene(14.24–11.54 Ma). This assemblage was dominated by epifaunal species with relative high diversity, suggesting high–energy, high–oxygenation and oligotrophic conditions with episodic supply of organic food. The dominant Cibicidoides spp. assemblage with high diversity, indicates a mesotrophic conditions with relative high–oxygen content during the Late Miocene to Pliocene(11.54–4.53 Ma). The appearance and continuous occurrence of Ammonia spp. and Pseudorotalia spp. since 10.02 Ma, may reflect the influence of the Kuroshio Current.

A Juvenile Specimen of Sauropodomorpha from the Lower Jurassic of China and a Brief Review of the Lufeng Sauropodomorph Fauna

An incomplete dinosaur skeleton,including a partial skull,recently discovered from the Lower Jurassic Lufeng Formation of Yunnan,China,is here reported.Apart from its small size,little anatomical evidence supports,a priori,the non-adult status of this new sauropodomorph specimen but osteohistological analyses suggest that it is a fast-growing juvenile.This specimen represents only the second occurrence of a juvenile non-sauropodan sauropodomorph in the Lufeng Basin.The anatomy of the new specimen does not match that of other Lower Jurassic immature specimens;although cranial material is preserved,it does not display the diagnostic characters of early sauropodomorphs from the same horizon,namely Lufengosaurus,Yizhousaurus and Yunnanosaurus.Our phylogenetic analysis places the new specimen in a position relatively distant from other Chinese sauropodomorphs,and corroborates the anatomical evidence showing it is not referable to any known species already excavated in Yunnan.This result is interpreted with caution considering that ontogeny affects phylogenetic reconstruction.A thorough comparison with adult forms,taking into account ontogenyrelated characters,suggests that this Lufeng juvenile might represent a previously unknown species of early sauropodomorph.

Differences of tuffaceous components dissolution and their impact on physical properties in sandstone reservoirs: A case study on Paleogene Wenchang Formation in Huizhou-Lufeng area, Zhu I Depression, Pearl River Mouth Basin, China

The element geochemical characteristics and diagenetic alteration products of tuffaceous components in sandstone reservoirs of Paleogene Wenchang Formation in typical subsags of the Huizhou-Lufeng area of the Zhu I Depression,Pearl River Mouth Basin,were identified through microscopic analysis and quantitative analysis of main and trace elements.The impacts of dissolution of different tuffaceous components on physical properties of reservoirs were discussed through quantitative characterization of reservoir physical properties.The results show that there are mainly four types of tuffaceous components in the study area,which are acidic,intermediate,basic and alkaline tuffaceous components.The acidic tuffaceous components evolved in a process of strong alteration and weak dissolution of alteration products,with a large amount of kaolinite precipitated during alteration to disenable the improvement of porosity and permeability.The intermediate and alkaline tuffaceous components evolved in a process of strong dissolution of tuffaceous components and strong alteration of residual tuffaceous components;the dissolution of tuffaceous components created intergranular pores,but the alteration products such as autogenic quartz,apatite and illite deteriorated the pore structure;ultimately,the dissolution of tuffaceous components resulted in the increase of porosity but no increase of permeability of the reservoir.The basic tuffaceous components dominantly evolved in a process of dissolution of tuffaceous components to strong dissolution of alteration products;both tuffaceous components between particles and laumontite generated from alteration can be strongly dissolved to create pores;thus,the dissolution of tuffaceous components can significantly increase the physical properties of the reservoir.

MODELLING OF COMPOSITION OF MANTLE SOURCE FOR THE JIJIE ALKALINE-ULTRABASIC INTRUSIVE COMPLEX, LUFENG, YUNNAN

Based on the data on petrology and geochemisty for the Jijie alkaline-ultrabasic intrusive rock complex, this paper, by means of correlation, suggested that the average composition of melteigites with 10% olivine added (Fo=86) can be considered as the composition of the primary magma of the Jijie complex. This magma, whose composition is estimated from the incompatible element P2O5, was produced by 3%±partial melting of pyrolites. The results of Petrological Mixing Calculating showed that the mantle-source rocks of the Jijie complex are obviously depleted in incompatible elements.

Geochemistry of Alkaline-Ultrabasic Rocks in the Jijie Complex, Lufeng, Yunnan

This paper is concerned with the geochemical features of major elements, transitionmetal elements, large ion lithophile elements, rare-earth elements and Sr isotopes in alkaline-ul-trabasic rocks in the Jijie complex of Lufeng, Yunnan Province, which is located in southernSichuan-Yunnan rift zone, one of Luoci alkaline-ultrabasic complexes in central Ynnnan.Moreover, its origin pertaining primary magma, magma soure region, fractional crystallization,etc. are also discussed in the present paper.

珠江口盆地陆丰凹陷西北洼原型盆地及迁移演化特征

陆丰凹陷西北洼是发育在珠一坳陷惠陆低凸起上的古近系残留型洼陷,总体表现为古近系“北断南削”型箕状半地堑和新近系坳陷型洼陷的双层结构特征,具有较好的油气勘探潜力。基于对研究区高精度三维地震的精细解释、平衡剖面恢复、洼陷结构和构造演化分析,揭示了研究区西段、中段和东段在原型盆地及其动力学机制、洼陷结构和构造演化、岩浆底侵期次及强度等方面存在显著的分段差异性,并表现出由东向西的迁移性演化特征。由东到西,洼陷变形机制由脆-韧性变形转变为脆性变形,洼陷伸展量、伸展率逐渐变大;岩浆底侵作用总体上东强西弱,强烈底侵期东早西晚;控洼断裂的滑脱作用东强西弱,滑脱时期东早西晚;早断陷期文下段沉积厚度总体上东厚西薄,晚断陷期恩下段西厚东薄;古近系地层翘倾、剥蚀作用总体上东强西弱,时间上东早西晚。结合研究区地温梯度及岩浆底侵作用的横向差异,提出了热机制是西北洼成盆机制及分段差异演化的主控因素,并导致了西北洼从东到西、由早到晚的迁移性演化特征。西北洼迁移性演化特征的新认识将对其石油地质条件分段差异性的深入研究及推动勘探进程提供科学指导。

Paleogene geological framework and tectonic evolution of the central anticlinal zone in Lufeng 13 sag,Pearl River Mouth Basin

The Paleogene geological framework and evolution process in the central anticline zone in the Lufeng 13 sag in Pearl River Mouth Basin is well analyzed through seismic data and drilling data,and control of tectonic evolution on hydrocarbon accumulation is also discussed.The results show that the central anticline zone in the Lufeng 13 sag develops the upper deformation layer and lower deformation layer.The“arched graben system”is developed in the upper deformation layer,and the magmatic diapir structure and flowing deformation of plastic strata is developed in the lower deformation layer.The evolution process of the central anticline zone can be divided into four stages,i.e.fault block uplifting stage,prototype stage,strengthening stage and finalization stage.The geological framework and tectonic evolution of the central anticline zone control Paleogene hydrocarbon accumulation.The Paleogene twolayer geological framework is favorable for development of structural traps and composite traps;the paleostructure highs are the direction of hydrocarbon migration,and the gravitational gliding faults are the main carrier bed for vertical hydrocarbon migration;the tectonic uplift is a key factor for reservoir diagenesis improvement and preservation of primary pores,and also controls distribution of high-quality reservoirs.

Tooth loss and alveolar remodeling in Sinosaurus triassicus (Dinosauria: Theropoda) from the Lower Jurassic strata of the Lufeng Basin, China

Pathological or traumatic loss of teeth often results in the resorption and remodeling of the affected alveoli in mammals. However, instances of alveolar remodeling in reptiles are rare. A remodeled alveolus in the maxilla of the Chinese theropod Sinosaurus (Lower Jurassic Lower Lufeng Formation) is the first confirmed example of such dental pathology in a dinosaur. Given the known relationship between feeding behavior and tooth damage in theropods (teeth with spalled enamel, tooth crowns embedded in bone) and the absence of dentary, maxillary, and premaxillary osteomyelitis, traumatic loss of a tooth is most likely the cause of alveolar remodeling. Based on the extent of remodeling, the injury and subsequent tooth loss were non-fatal in this individual.

基于信息量模型的云南禄丰地质灾害风险性评价

禄丰市位于云南省中部,区内地质环境复杂,地质灾害多发频发,严重威胁当地居民生命财产安全。以禄丰市为研究区,结合1∶5万地质灾害风险调查数据,基于GIS平台,采用信息量模型,构建以栅格为单位的风险评价方法。针对不同灾害类型,选取不同评价因子进行地质灾害易发性评价;基于评价结果,以近10年汛期月(5—10月)累计平均降水量为诱发因素,开展危险性评价;选取建筑物、人口和交通设施分布等因子构建承灾体的易损性评价模型;根据危险性和易损性评价结果,利用矩阵分析方法完成区内风险评价。结合区内地质灾害易发程度、承灾体情况、险情等级及地质灾害防治能力,实现研究区地质灾害风险性区划。结果显示,区内地质灾害高风险区主要分布于恐龙山镇-妥安乡龙川江沿岸,面积为290.47 km^(2),占比8.16%;中风险区主要分布于高峰乡、彩云镇,面积为2044.21 km^(2),占比57.48%;低风险区主要分布于妥安乡至高峰乡、金山镇、中村乡等地势平缓地带,面积为1222.05 km^(2),占比34.36%。评价结果可为禄丰市地质灾害防治减灾提供依据,并为其他地区开展评价提供思路和参考。

珠江口盆地陆丰南地区文昌组沉积古环境恢复及烃源岩有机质富集主控因素研究

文昌组为陆丰南地区主力烃源岩发育层段,为了恢复文昌期沉积古环境,探讨优质烃源岩有机质富集主控因素,选用166组文昌组泥岩样品的主、微量元素测试数据,采用元素地球化学方法,在研究区首次详尽分析文昌期不同次洼、不同层段的古盐度、古气候、古水深和古氧相的纵横向演变规律,并探讨部分钻井出现盐度异常的原因及三芳甲藻甾烷、球藻对古环境的指示意义,结合TOC、古生产力和陆源输入变化研究,明确了研究区优质烃源岩的主控因素。结果表明:陆丰南地区始新统文昌组沉积期水体以淡水环境为主,局部层段盐度微弱增加,垂向上,从文四段向文一+二段水体盐度逐渐降低,横向上,文四段沉积期,陆丰15洼水体盐度最高,文三段—文一+二段沉积期,陆丰13东洼水体盐度较高。推测陆丰南地区文昌组水体盐度变化受到海侵影响,文四段沉积期,海侵影响主要集中在陆丰15洼,文三段沉积期,海侵影响扩大至陆丰15洼和陆丰13东洼东侧,进入文一+二段沉积期,受海侵影响程度较小。球藻及三芳甲藻甾烷在研究区不能作为水体咸化或者海侵的判别指标,球藻含量变化与古气候、古生产力、古水深关系密切,受古盐度变化影响有限。陆丰南地区文四段沉积期古气候温湿,古水深最大,还原性最强,进入文三段、文一+二段,气候温湿程度、水深和还原性均有所降低;文四段沉积期陆丰13东洼水深最大,其次为陆丰15洼,还原性陆丰13东洼最强,其次为陆丰13西洼。文昌组烃源岩有机质富集主要受控于古生产力和古陆源输入,其次受古气候和古水深控制,古氧相变化对有机质富集控制作用较弱,高古生产力主导着文昌组优质烃源岩的形成及分布,主要发育生产力富集模式。

双酶法优化禄丰香醋糖化工艺

为提高禄丰香醋的生产效率,通过添加α-淀粉酶与糖化酶,对禄丰香醋生产过程中糖化工艺进行优化。糖化工艺包括液化工艺与糖化工艺两部分:液化实验以还原糖为指标;糖化实验以还原糖为主要指标,黄酮类物质、氨基酸态氮为次要指标。在单因素实验的基础上,采用响应面分析法对禄丰香醋糖化过程中的参数进行优化。研究结果表明,禄丰香醋的最佳糖化工艺参数为α-淀粉酶添加量2.272%、液化pH 4.9、液化温度50℃、液化时间43 min,此条件下还原糖含量为5.372 g/100 g。结合实际生产情况,当糖化酶添加量为2.336%、糖化pH为4、糖化温度为55℃、糖化时间为60 min、蒸煮时间为1 h、料液比为1∶3时得到还原糖含量为13.614 g/100 g,黄酮含量为6.867 mg/L,氨基酸态氮含量为0.101724 g/dL。

陆丰油田古近系低渗高温深层储层自源闭式强化注水技术研究与应用

受海上平台空间、作业成本、注水水源、施工工艺等条件限制,如何高效注水开发陆丰油田古近系低渗高温深层储层面临挑战。以陆丰油田古近系储层试验井为例,开展了注水可行性分析,优选了合适的水源层位和注入层;采用了同井自源类水层补充地层能量的自源闭式注水工艺,研发的配套配水器可满足调节扭矩≤5 N·m、耐压差35 MPa,测调仪器可满足耐温175℃、耐压60 MPa的性能要求,实现了海上平台深层一井多用、无须地面设备的注水新方式;采用了电缆传输的爆燃压裂工艺,实现快速、高效作业,措施的时间控制在14 h以内,时效提高10倍以上,火药密度超过6 kg/m;通过强溶缓速酸酸化复合增效。自源闭式强化注水技术已在陆丰油田试验井M10井取得成功应用,注水高效,受效井增产降水效果明显。本文研究成果有效拓展了注水技术在低渗、深层、高温储层中的应用,可为类似储层规模开发提供借鉴。

惠陆低凸起东侧早文昌期源-汇系统分析与勘探实践

惠陆低凸起东侧为陆丰南富生烃洼陷,为厘清该低凸起东侧物源面貌及沉积储层分布规律,综合利用钻井和三维地震资料,恢复了古物源区面貌,描述了源-汇体系要素,预测了富砂沉积体平面分布,并探讨了砂体差异富集的控制因素。结果表明:惠陆低凸起发育完整的受古地貌控制的源-汇系统,研究区古近纪下文昌组进一步可划分为A—H共8个凸起群单元,在古地貌恢复的基础之上,8个凸起群单元共划分出17个由独立流域和对应沉积区组成的源-汇系统。惠陆低凸起东侧发育流域1—6组成的6个独立的源-汇系统,其中流域2、4和6剥蚀范围大,基底受剥蚀能力强,水系发育数量多且相对汇聚,是主要的优势物源供给区。2号流域(陆丰13东洼缓坡中部)大的剥蚀面积、花岗岩和喷出岩母岩为大型辫状河三角洲及优势储层发育提供了物质基础,多个水系和平面上的优势汇聚为优质的水下分流河道砂岩储层提供了良好的发育条件。

不同贮藏年份禄丰香醋细菌多样性分析

采用高通量测序技术对4个不同贮藏年份(2017、2018、2019、2020年)禄丰香醋的细菌多样性进行分析测定。结果表明,不同贮藏年份样品中的细菌菌群组成差别较大;2017、2018、2019年的细菌菌群多样性更高,主要优势菌门分别为厚壁菌门(Firmicutes)、变形菌门(Proteobacteria)、放线菌门(Actinobacteriota);优势细菌属主要为草螺菌属(Herbaspirillum)、不动杆菌属(Acinetobacter)、肥杆菌属(Hafnia-Obesumbacterium)、肠杆菌属(Enterobacter)、包西氏菌属(Bosea)。而2020年的优势菌门主要为厚壁菌门(Firmicutes)、变形菌门(Proteobacteria);优势细菌属主要为乳杆菌(Lactobacillus)、罗尔斯通氏菌(Ralstonia)、乳酸杆菌(Lactobacillus_homohiochii)。线性判别分析效应大小分析和相关性分析都表明细菌菌群的多样性与贮藏时间有关,京都基因与基因组百科全书预测分析表明,禄丰香醋中的有益菌群在初级代谢与次级代谢之间起着重要作用,之后可以进一步深入研究。本研究发现了不同贮藏年份禄丰香醋中细菌菌群多样性的变化,为禄丰香醋细菌多样性分析、优质菌种资源选育及发酵食醋工业化生产奠定了基础。

基于地质工程一体化的海上低渗油田压裂实践与认识——以珠江口盆地陆丰凹陷为例

珠江口盆地作为中国海上低渗油气的重要成藏区,低渗油气资源量巨大。陆丰凹陷L44油田是南海东部首个整装压裂开发的低渗油田,为提升开发效益,采用压裂等储层改造方式,但压裂后存在改造规模未达预期、裂缝起裂机理认识不清等问题。建立了一种基于地震解释、测井、地质相结合的海上低渗油田地质工程一体化建模方法,使裂缝扩展延伸更加准确。对研究区开展了三维地质力学建模和地质工程双甜点优选,提出了适用于海上低渗油田压裂设计的储层射孔段长度上限,对C3井重新进行了压裂方案设计和产能模拟,经二次压裂投产后产量水平与设计预期基本相符。研究结果表明:(1)低排量条件下,射孔段长度由4m增至16m,单段裂缝长度平均减少30m,前5年单井累计产能减小88%;(2)射孔段长度的增大对改造规模起到抑制作用,射孔段长度大于6m时,改造范围大幅减小,射孔段长度小于6m时,改造范围减小幅度不大,最优射孔段长度不应大于6m;(3)射孔段长度小于6m时,施工排量每提升1m^(3)/min,储层改造体积平均增幅为10.97%,提高施工排量可实现进一步增大压裂改造体积的目标。建立的海上低渗油田地质工程一体化建模方法为南海东部低渗油田的开发方案和压裂方案设计提供了全新认识,有利于提升油田开发效益。

陆丰海域秋季第一模态内孤立波观测特征分析

南海北部内孤立波异常活跃,具有极强的非线性、极高的强度和极大的能量,其传播特性和精细结构在背景过程影响下更加复杂,加剧了内孤立波预报和海上石油平台作业的难度。基于南海北部陆丰海域295 m水深处一套潜标连续79 d的观测资料,分析了秋季内孤立波的波动特征和统计规律。典型内孤立波表现为波列的形式,头波振幅达86.7 m,在海洋上层导致局地增温超过8.0℃,并诱发最大达0.83 m/s的西向流和0.60 m/s的北向流,在波前产生最大达0.25 m/s的下降流。对观测期间捕捉到的91个内孤立波统计分析表明,内孤立波主要沿WNW方向传播,平均振幅为59.9 m,在海洋上层诱发的最强西向流速平均值为0.79 m/s;在天文大潮时期,内孤立波在04:00至06:00和16:00至19:00频繁出现,且农历初二至初五和十六至十八期间经过陆丰海域的内孤立波具有更大的强度。此外,全日内潮与半日内潮共同作用下压了温跃层,导致典型内孤立波中形成了1个上凸波动,其在近底层导致局地降温达1.3℃,并诱发超过0.30 m/s的西向流和0.20 m/s的北向流;该上凸波动陡峭的波前汇聚了强剪切,极易触发剪切不稳定。本研究结果可为陆丰海域海上石油平台施工、勘探船作业等提供重要参考。

砂岩储层中凝灰质溶蚀效应的物理模拟实验研究——以珠江口盆地惠州—陆丰地区古近系文昌组为例

为认识埋藏过程中酸性流体对碎屑岩储层中凝灰质的溶蚀改造效应及控制因素,选取珠江口盆地珠一坳陷惠州—陆丰地区古近系文昌组凝灰质砂岩储层,设计开展了岩心尺度的流体—岩石相互作用模拟实验。通过显微镜下观察、流体成分分析、物性表征等方法,对比分析了实验前后不同流体流速、不同凝灰质含量条件下砂岩储层的溶蚀作用和物性响应特征。结果表明,酸性流体环境中凝灰质溶蚀现象普遍,但不同实验条件下,凝灰质溶蚀强度及储层物性响应不同:成岩体系的开放性与封闭性决定凝灰质的溶蚀作用强弱。相同岩石和相同酸性流体条件下,高流速开放体系中凝灰质溶蚀量高于封闭体系,且低流速相对封闭体系中溶蚀产物趋于沉淀,溶蚀作用增孔效应有限。凝灰质含量显著影响溶蚀效应,富凝灰质砂岩中溶蚀作用有限,含凝灰质砂岩和贫凝灰质砂岩能够溶蚀增孔,且含凝灰质砂岩的溶蚀增孔效率更高。凝灰质含量相对中等—较低的储层中,中浅层埋藏阶段的开放成岩流体体系最有利于粒间凝灰质溶孔的发育。经历晚期酸性流体溶蚀改造后,较易形成次生溶蚀型优质储层,这一认识有助于不同地区的溶蚀型储层甜点预测。