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| 1 | Differential Hydrocarbon Enrichment and its Main Controlling Factors in Depressions of the Bohai Bay Basin Differential Hydrocarbon Enrichment and its Main Controlling Factors in Depressions of the Bohai Bay Basin显示文摘Significant differential hydrocarbon enrichment occurs in depressions in a petroliferous basin.There are multiple depressions in the Bohai Bay Basin, and each depression as a relatively independent unit of hydrocarbon generation, migration and accumulation, contains significantly different hydrocarbon generation conditions and enrichment degree. On the basis of previous documents and a large number of statistical data, this work comparatively analyzed the differential hydrocarbon enrichment and its major controlling factors in depressions of the Bohai Bay Basin. The results show that depressions in the Bohai Bay Basin have various hydrocarbon enrichment degrees, and can be categorized into four types, namely enormously oil-rich, oil-rich, oily and oil-poor depressions. In general, the enormously oil-rich and oil-rich depressions are distributed in the eastern part of the basin along the Tan-Lu and Lan-Liao faults, whereas depressions in the western part of the basin are poor in hydrocarbons. Moreover, the vertical distribution of hydrocarbons is also highly heterogeneous, with Pre-Paleogene strata rich in hydrocarbons in the northern and western depressions, Paleogene strata rich in hydrocarbons in the entire basin, and Neogene strata rich in hydrocarbons in the off-shore areas of the Bohai Bay Basin. From early depressions in onshore areas to the late depressions in offshore areas of the Bohai Bay Basin, the source rocks and source-reservoir-cap rock assemblages gradually become younger and shallower, and the hydrocarbon resource abundance gradually increases. Hydrocarbon supplying condition is the key factor constraining the hydrocarbon enrichment for different depressions,while the main source-reservoir-cap rock assemblage, sufficient hydrocarbons and the transportation capacity of faults control the vertical distribution of hydrocarbons. The main factors controlling hydrocarbon enrichment are different for different layers. The hydrocarbon supplying condition of source rocks is the key controlling factor, whereas the source-reservoir configuration, the main sourcereservoir-cap rock assemblages, and the fault transportation are the main factors of hydrocarbon enrichment in the Paleogene, Paleogene and Neogene, respectively. | JIANG Youlu LIU Hua SONG Guoqi WANG Yongshi LIU Jingdong ZHAO Kai LYU Xueying | 2017 | Acta Geologica Sinica(English Edition)2017，91，5： | 15 |
| 2 | Relationship between Geological Structures and Hydrocarbon Enrichment of Different Depressions in the Bohai Bay Basin显示文摘The Bohai Bay Basin contains many depressions with varying degrees of hydrocarbon enrichment associated with the geological structures of different depressions. This study discussed the relationship between the geological structures and hydrocarbon enrichment of the depressions in the Bohai Bay Basin. Based on the Paleogene strata distribution and the length to width ratio of different depressions, their geological structures are divided into three types in plan-view: open(length/width < 2), narrow(length/width > 4) and transitional types(length/width 2–4). In cross section, the geological structures can be divided into dustpan I, dustpan II and double-faulted types. Based on tectonic evolution and sedimentary characteristics, the depressions are classified into early-formed, inherited and late-formed categories. Generally, narrow depressions are mainly located in the northeast and southwest of the Bohai Bay Basin, while open depressions are dominantly distributed in the central area of the basin; late-formed depressions are mainly around the Bohai sea area, and early-formed depressions are mostly located in the periphery of the basin. Geological structures of the depressions control the formation of the source, reservoir and cap rocks as well as hydrocarbon accumulation setting, and further influence the pay zones and oil-bearing sequence. In detail, dustpan II and doublefaulted depressions mainly have A-type sags, which often possess better hydrocarbon generation conditions than dustpan I ones; hydrocarbons in open dustpan II depressions tend to accumulate in the central uplift areas or buried hill, while those in narrow dustpan I depressions always accumulate in gentle slope belts. The oil-bearing sequence for different evolutional depressions corresponds well with the sedimentary strata of the main development stages of depressions. In early-formed depressions, hydrocarbons are mainly enriched in deeply buried reservoirs, while in late-formed depressions hydrocarbons are abundant in the relatively shallow traps. In summary, most inherited and late-formed dustpan II depressions are enriched in hydrocarbons due to their extensive source rocks and good source–reservoir–seal assemblages, whereas dustpan I and early-formed depressions are relatively poor in hydrocarbons. | JIANG Youlu LIU Hua SONG Guoqi WANG Yongshi LIU Pei Lü Xueying | 2015 | Acta Geologica Sinica(English Edition)2015，89，6： | 13 |
| 3 | A Discussion on the Origin of Shale Reservoir Inter-Laminar Fractures in the Shahejie Formation of Paleogene, Dongying Depression显示文摘This paper was conducted on the shale reservoir in the Dongying depression in the Shahejie Formation of Paleogene. Based on detailed core description, rock thin sections, argon ion polishing, scanning electron microscopy(SEM) analysis, CT scanning and carbon-oxygen isotopic test, the formation mechanism of the inter-laminar fractures(or seams) and their development conditions were discussed by comprehensive analysis of the diagenetic evolution features and the reservoir space evolution characteristics. The results show that the laminated composite pattern in Dongying depression was dominated by vertical distribution of laminated calcite and clay minerals. Contrasted to the traditional understanding, development degree of inter-laminar fractures was much lower. Pure fluid between layers cannot exist without framework minerals, and the pre-existing well connected pore or horizontal overpressure micro seam was favorable paths of fluid migration. From the points of inter-laminar fractures origin mechanism and its evolution, the so called seams, were much more complex than traditional understanding that hydrocarbon generation raised the pore pressure and led to the parallel microfractures. But the inter-laminar fractures had little relationship with that whether the lamination was developed or bedding boundary was clear or not. In fact, the shale reservoir inter-laminar fractures were not rigorous fracture. They were controlled by pre-existing inter-granular pore(or seam) or dissolved pore, which distributed along carbonate laminae boundary and were connected by later super pressure, dissolution and the seepage force. And the development conditions were burial depth(bigger than 3 000 m) and the Ro value(>0.6%). Discussion on its origin and evolution has important petroleum geological significance on optimizing reservoir segment and favorable target areas selection. | Huimin Liu Shun Zhang Guoqi Song Shoupeng Zhang Xuefeng Hao Zhonghuai Xie Ningning Xu Peng Liu | 2017 | Journal of Earth Science2017，28，6： | 10 |
| 4 | Geobiological processes of the formation of lacustrine source rock in Paleogene显示文摘Gypsum-salt rocks and coccolith calcareous shale are widely deposited in the lower part of the Paleogene Shahejie Formation in the Dongying Sag,Shandong Province.The gypsum-salt rock is believed to be formed during the earlier deposition in salt lake,while the overlying coccolith shale in saline lake with relatively low salinity.By comparing the lake environment and lacustrine microbial communities between ancient and recent lakes,cyanobacteria are regarded as the main representative of productivity during the formation of gypsum-salt strata series,with the annual productivity of 1500-2000 gC m-2 yr-1.Based on the research of ultramicrofossils in the calcareous shale,coccolith is considered as the main contributor to the productivity during the formation of calcareous shale.On the basis of statistic data of sedimentary rates,shale laminations,and coccolith fossils in each lamination,the quantitative value of productivity is calculated,with the annual productivity of 2250-3810gC m-2 yr-1(averagely 3120 gC m-2 yr-1).Statistic data of large amount of pyrite framboids indicate that the lower water column was persistently in sulfidic or anoxic conditions during the deposition of gypsum-salt strata series,but it changed to be dysoxic when the coccolith calcareous shale was deposited.Both of these water conditions are favorable for the preservation of organic matter.It is estimated that the organic carbon burial efficiency of the Lower Paleogene salt lakes and saline lakes of Dongying Depression is about 10%-15%,which is calculated and analyzed using the multi-parameter geobiological model. | LI GuoShan WANG YongBiao LU ZongSheng LIAO Wei SONG GuoQi WANG XueJun XU XingYou | 2014 | Science China Earth Sciences2014，57，5： | 10 |
| 5 | Diagenetic Evolution and Formation Mechanisms of High-Quality Reservoirs under Multiple Diagenetic Environmental Constraints:An Example from the Paleogene Beach-Bar Sandstone Reservoirs in the Dongying Depression,Bohai Bay Basin显示文摘The diagenetic environment, diagenetic responses, diagenetic transformation model and formation mechanisms of high-quality reservoirs(beach-bar sandstones of the Paleogene fourth member) in the Dongying depression were studied through the analysis of fluid inclusions, thin section and burial evolution history. The diagenetic fluids of the beach-bar sandstone reservoirs evolved from early high salinity and weak alkalinity to low salinity and strong acidity, late high salinity and strong alkalinity and late low salinity and acidity, which were accompanied by two stages of oil and gas filling. The fluids at the margins of the sandbodies were continuously highly saline and strongly alkaline. The western(eastern) reservoirs experienced early open(closed), middle open, and late closed diagenetic environments during their burial history. The flow pattern was characterized by upwelling during the majority of the diagenesis(in the east, a non-circulating pattern transitioned into an upwelling current). Due to the evolution of the diagenetic fluids, the diagenetic sequence of the beach-bar reservoirs was as follows: early weak carbonate cementation; feldspar and carbonate cement dissolution and authigenic quartz cementation; late carbonate and anhydrite cementation, authigenic feldspar cementation, and late quartz dissolution; and late carbonate cementation, feldspar dissolution, and authigenic quartz cementation. The diagenetic strength during these stages varied or was absent altogether in different parts of the reservoirs. Due to the closeness of the diagenetic environment and the flow pattern of the diagenetic fluids, the diagenetic products are variably distributed in the sandstones interbedded with mudstones and in the fault blocks. The evolution of multiple alternating alkaline and acidic diagenetic environments controlled the distribution patterns of the reservoir diagenesis and reservoir space, and the reservoir quality index, RQI, increased gradually from the margins to the centers of the sandstones. The closeness of the diagenetic environment and the flow patterns of the diagenetic fluids controlled the differences in the reservoir properties among the fault blocks. With increasing distance from the oil-source faults, the RQI values in the west gradually decreased and in the east initially increased and then decreased. | WANG Jian CAO Yingchang SONG Guoqi LIU Huimin | 2017 | Acta Geologica Sinica(English Edition)2017，91，1： | 5 |
| 6 | Postnatal calpeptin treatment causes hippocampal neurodevelopmental defects in neonatal rats显示文摘Our previous studies showed that the early use of calpain inhibitors reduces calpain activity in multiple brain regions, and that postnatal treatment with calpeptin may lead to cerebellar motor dysfunction. However, it remains unclear whether postnatal calpeptin application affects hippocampus-related behaviors. In this study, Sprague-Dawley rats were purchased from the Animal Center of Anhui Medical University of China. For the experiments in the adult stage, rats were intraperitoneally injected with calpeptin, 2 mg/kg, once a day, on postnatal days 7–14. Then on postnatal day 60, the Morris water maze test was used to evaluate spatial learning and memory abilities. The open field test was carried out to assess anxiety-like activities. Phalloidin staining was performed to observe synaptic morphology in the hippocampus. Immunohistochemistry was used to count the number of NeuN-positive cells in the hippocampal CA1 region. DiI was applied to label dendritic spines. Calpeptin administration impaired spatial memory, caused anxiety-like behavior in adulthood, reduced the number and area of apical dendritic spines, and decreased actin polymerization in the hippocampus, but did not affect the number of NeuN-positive cells in the hippocampal CA1 region. For the neonatal experiments, neonatal rats were intraperitoneally injected with calpeptin, 2 mg/kg, on postnatal days 7 and 8. Western blot assay was performed to analyze the protein levels of Akt, Erk, p-Akt, p-Erk1/2, Erk1/2, SCOP, PTEN, mTOR, p-mTOR, CREB and p-CREB in the hippocampus. SCOP expression was increased, and the phosphorylation levels of Akt, mTOR and CREB were reduced in the hippocampus. These findings show that calpeptin administration after birth affects synaptic development in neonatal rats by inhibiting the Akt/mTOR signaling pathway, thereby perturbing hippocampal function. Therefore, calpeptin administration after birth is a risk factor for neurodevelopmental defects. | Zhu-Jin Song San-Juan Yang Lan Han Bin Wang Guoqi Zhu | 2019 | Neural Regeneration Research2019，14，5： | 5 |
| 7 | Analysis of petrophysical cutoffs of reservoir intervals with production capacity and with accumulation capacity in clastic reservoirs显示文摘Methodologies have been developed for calculating cutoffs of reservoir intervals with production capacity(RIPC) and reservoir intervals with accumulation capacity(RIAC) according to the types of pore throat structures and dynamic force by using data from petrophysical analysis, production tests and mercury injection. The data are from clastic reservoirs in the third member(Es3) and the fourth member(Es4) of the Shahejie Formation in the Shengtuo area on the North Slope of the Dongying Sag, Jiyang Depression, China. The method of calculating cutoffs of RIPC is summarized as follows: 1) determination of permeability cutoffs of RIPC; 2) classification of types of pore-throat structures according to mercury injection data and then relating porosity to permeability and determining the relationship between porosity and permeability according to each type of pore-throat structure; and 3) calculating porosity cutoffs of RIPC using established correlation between porosity and permeability according to the type of pore throat structure. The method of calculating cutoffs of RIAC includes: 1) establishing a functional relationship between oil-water interfacial tension and formation temperature; 2) calculating limiting values of maximum connected pore-throat radii according to formation temperature and dynamic forces of each reservoir interval; 3) correlating permeability with maximum connected pore-throat radius and then obtaining permeability cutoffs of RIAC; and 4) calculating porosity cutoffs on the basis of permeability cutoffs according to specific correlations, suitable for the type of porethroat structure. The results of this study show that porosity and permeability cutoffs of clastic reservoirs decrease with depth. For a fixed permeability cutoff, the porosity cutoff of RIPC varies because the type of pore throat is different. At a fixed temperature, porosity and permeability cutoffs of RIAC decrease as dynamic force increases. For a fixed permeability cutoff of effective hydrocarbon accumulation, the porosity cutoff also varies with different types of pore throat. | Wang Yanzhong Cao Yingchang Song Guoqi Song Ling Yang Tian Zhang Shaomin | 2014 | Petroleum Science2014，11，2： | 4 |
| 8 | Characteristics and Genetic Mechanisms of Overpressure in the Depressions of Bohai Bay Basin, China显示文摘The distribution and genetic mechanisms of abnormal pressures in the Bohai Bay Basin were systematically analyzed. Abnormal pressures are widely developed in the Bohai Bay Basin,primarily in the Paleogene E_(2s_4),E_(2s_3),E_(s_1),and Ed formations. From the onshore area of the Bohai Bay Basin to the center of the Bozhong area,the top depth of the overpressured zone in each depression increases gradually,the overpressured strata in each depression gradually move to younger formations,and the pressure structure successively alters from single-bottom- overpressure to doublebottom-overpressure and finally to double-top-overpressure. The distribution of overpressured area is consistent with the sedimentary migration controlled by the tectonic evolution of the Bohai Bay Basin,which is closely related to the hydrocarbon-generation capability of active source rocks. The overpressured strata are consistent with the source-rock intervals in each depression; the top of the overpressured zone is synchronous with the hydrocarbon generation threshold in each depression; the hydrocarbon generation capability is positively correlated with the overpressure magnitude in each formation. Undercompaction was the main mechanism of overpressure for depressions with fluid pressure coefficients less than 1.2,whereas hydrocarbon generation was the main mechanism for depressions with fluid pressure coefficients greater than 1.5. | LIU Hua JING Chen JIANG Youlu SONG Guoqi YU Qianqian FENG Yuelin | 2016 | Acta Geologica Sinica(English Edition)2016，90，6： | 4 |
| 9 | Vermicular fossils in the Early Cambrian Xidashan Formation in the Quruqtagh region of Xinjiang, China显示文摘大量蠕虫状的石块和海绵动物石块的次要的数量在 Quruqtagh 的区域在早寒武纪的 Xidashan 形成被发现了, Xinjiang。蠕虫状的石块通常是长的超过 50 公里和 0.3-1.4 公里宽;他们的起皱的 lamellae 是有在长度以内的 3-10 片的微罚款每每毫米。石块被认为是 Sabellidites cambriensis Sokolov (1965 ) 。Xidashan 形成是在 Sabelliditesoccur 的最高的阶层是到目前为止报导了。 | YANG Ruidong ZHANG Chuanlin SONG Guoqi LUO Xinrong | 2006 | Progress in Natural Science:Materials International2006，16，5： | 3 |
| 10 | Interaction between source rock and evaporite:A case study of natural gas generation in the northern Dongying Depression显示文摘It is well known that oil generated from source rocks of saline-lake facies is characteristic of low Pr/Ph ratio and high contents of gammacerane.The authors found that gas generated from the same source rocks was high in benzene and cyclohexane contents and had light carbon isotope compositions.In this study,a series of thermal simulations of gas generations on source rock with/without evaporites(such as carbonate,gypsum,and sodium chlorite,respectively),were conducted.It was found that the gypsum played an important role on the catalyzsis of gas generation in the thermal simulations.Compositions of the gaseous hydrocarbons generated from source rocks with evaporites are very similar to those of natural gases discovered from northern Dongying Depression.Meanwhile,in the thermal simulations,it was found that the carbon isotopic compositions of gaseous hydrocarbons generated from source rocks with evaporites are lighter than those of the gases from source rocks without evaporites.Therefore,it is concluded that natural gases discovered from northern Dongying Depression are the product of interaction between source rocks and evaporites(especially gypsum) of the saline facies. | JIN Qiang WANG Juan SONG Guoqi WANG Li LIN Lamei BAI Shengpin | 2010 | Chinese Journal Of Geochemistry2010，29，1： | 3 |
| 11 | Sedimentation in a Continental High-Frequency Oscillatory Lake in an Arid Climatic Background:A Case Study of the Lower Eocene in the Dongying Depression,China显示文摘The sedimentary environment,formation conditions,sedimentary characteristics and the basin evolution model of high-frequency oscillatory lake in arid climatic background of the Lower Eocene in the Dongying depression were studied through the analysis of drilling cores,sporepollen,geochemistry and geophysics data.During the sedimentary period of the Eocene Ek1–Es4x formations,because of the frequent alternation between dry and wet climates in the arid climatic background and the gentle paleogeomorphology,the lake level and salinity of the Early Eocene Dongying depression frequently and rapidly increased and decreased,which is referred to as a high-frequency oscillatory lake.The sedimentation and distribution of sediments in this high-frequency oscillatory lake basin were controlled by the frequently alternating dry-wet climates.During periods with relatively wet climate,the seasonal floods and unstable rivers led to the formation of over-flooding lake deltas in the gentle slope belt,and fine-grained clastic sediments,with minor thin layers of gypsum-salt rocks in the sag belt.During the relatively arid climatic periods,sedimentation occurred mainly in the limited area of the sag belt with thick gypsum-salt rocks.Because of the impact of the salinity stratification of the lake water,these gypsum-salt rocks exhibit annular structural features.A sedimentary cycle of the oscillatory lake began with isochronous flood channels and ended with relatively thick gypsum rocks and salt rocks.The thickness of one oscillatory cycle is generally 4–20 m.The superposition of multiple sedimentary cycles of the oscillatory lake constitutes the overall vertical filling sequence of the high-frequency oscillatory lake basin. | Jie Liu Jian Wang Yingchang Cao Guoqi Song | 2017 | Journal of Earth Science2017，28，4： | 2 |
| 12 | Relationship between heterogeneity of source rocks and genetic mechanism of abnormally high pressure显示文摘Based on the micro-fluorescence observation of polished sections of source rocks,two types of micro-layers with different wetting properties formed in thermal evolution,i.e.,oil-wetting and water-wetting micro-layers,are distinguished.The wetting property is found closely related to the abundance of organic matter and its occurrences with inorganic minerals.The alternating distribution and intercrossing of two types of micro-layers formed many separated spaces with different wettabilities.The strong capillary forces in these separated spaces with different wettibilities obstruct the cross flows of pore fluids and result in nearly independent and closed fluid systems.As a consequence,these spatially superposed spaces in source rocks bear the overburden pressure and then abnormally high pressures have developed in the whole source rock unit.Therefore,the abundance and occurrences of organic matter are the main inner factors influencing the formation of abnormally high pressures,whereas the formation,distribution and development of micro-layers with different wettabilities during the evolution of source rock determine the intensity and spatial distribution of abnormally high pressures. | ZHANG XueJun XU XingYou WANG YongShi SONG GuoQi GUO ChunQing LIU Qing LI Ping | 2013 | Science China Earth Sciences2013，56，11： | 1 |
| 13 | Fault control on hydrocarbon migration and accumulation in the tertiary Dongying Depression,Bohai Basin,China显示文摘 | Lampe C Song Guoqi Cong Liangzi | 2012 | AAPG Bulletin2012，96，6： | 1 |
| 14 | Formation mechanism of carbonates in the lacustrine muddy shale and it implication for shale oil and gas: A case study of source rocks in Member 4 and Member 3 of Shahejie Formation, Dongying sag显示文摘Through analysis of microscopic characteristics,mineral components,elements and isotopes,the genetic mechanism of carbonates in the deep lacustrine source rocks in the upper submember of Member 4 and lower submember of Member 3 of Shahejie Formation in Dongying sag,is well investigated.The results show that four types of carbonates in the deep lake,i.e.,lenticular coarse crystalline carbonate,lamellar micro-fine crystalline carbonate,lamellar cryptocrystalline carbonate and massive cryptocrystalline carbonate.Of which,the lenticular coarse crystalline carbonate is formed by diagenetic recrystallization.For the lamellar micro-fine crystalline carbonate and the lamellar cryptocrystalline carbonate,through the alga photosynthesis,the carbon dioxide(CO_(2))is constantly extracted from water,thus the concentration of CO_(3)^(-2) ion in water increases,and then the CO_(3)^(-2) ion reacts with Ca2+ ion in lake water surface to form the carbonates;the saline water environment is favorable for preservation of carbonate particles which mostly occur in lamellar micro-fine crystalline;in the brackish water environment,the water is deep,and the carbonate crystalline beneath the carbonate compensation depth surface is usually is dissolved,and most of lamellar cryptocrystalline are preserved.The massive cryptocrystalline carbonate is formed by the sedimentary carbonate which transport from shallow water to deep water by gravity flow.To some extent,the carbonates control reservoir property and compressibility of muddy shale in the upper submember of Member 4 and lower submember of Member 3 of Shahejie Formation in Dongying sag,and provide important information for reconstruction of sedimentary environment of the ancient lake. | Yong Wang Huiming Liu Guoqi Song Xuefeng Hao Deshun Zhu Deyan Zhu | 2018 | Petroleum Research2018，3，3： | 1 |
| 15 | Fault control on hydrocar- bon migration and accumulation in the Tertiary Dongying depression, Bohai basin,China显示文摘 | Lampe C Song Guoqi Cong Liangzi | 2012 | AAPG Bulletin2012，96，6： | 1 |
| 16 | Early Paleozoic tectonic evolution of the Chinese South Tianshan Orogen: constraints from SHRIMP zircon U–Pb geochronology and geochemistry of basaltic and dioritic rocks from Xiate, NW China显示文摘 | Qing Qian Jun Gao Reiner Klemd Guoqi He Biao Song Dunyi Liu Ronghua Xu | 2009 | International Journal of Earth Sciences2009，，3： | 1 |
| 17 | Early Paleozoic tectonic evolution of the Chinese South Tianshan Orogen: constraints from SHRIMP zircon U–Pb geochronology and geochemistry of basaltic and dioritic rocks from Xiate, NW China显示文摘 | Qing Qian Jun Gao Reiner Klemd Guoqi He Biao Song Dunyi Liu Ronghua Xu | 2009 | International Journal of Earth Sciences2009，，3： | 1 |
| 18 | Comparative proteomic analysis of cold responsive proteins in two wheat cultivars with different tolerance to spring radiation frost显示文摘Spring radiation frost(SRF)is a severe environmental stress which impairs wheat yield and productivity worldwide.To better understand the mechanism of wheat(Triticum aestivum)responding to SRF,a comparative proteomic analysis was performed to analyze the changes of the key proteins in two wheat cultivars Jimai22 and Luyuan301 with high and low tolerance to SRF respectively.A total of 43 differentially expressed proteins(DEPs)which mainly involved in carbohydrate metabolism,amino acid metabolism,resistance proteins and antioxidant enzymes,photosynthesis and cellular respiration proteins,cell-wall related proteins,protein translation/processing/degradation and signal transduction were isolated and identified by two-dimensional electrophoresis and MALDI-TOF-TOF MS.The results revealed that of the 21 DEPs in Jimai22 responding to the SRF,13 DEPs were upregulated and 8 DEPs were downregulated,and that of the 22 DEPs in Luyuan301,9 DEPs were upregulated and 13 DEPs were downregulated.These DEPs might be responsible for the stronger cold resistance of Jimai22 compared to Luyuan301.The expression pattern and function analysis of these DEPs were very significant to understanding the mechanism of the SRF responses in wheat. | Shujuan ZHANG Guoqi SONG Yulian LI Jie GAO Jiao WANG Guiju CHEN Haosheng LI Genying LI Zhendong ZHAO | 2014 | Frontiers of Agricultural Science and Engineering2014，1，1： | 1 |
| 19 | Fault control on hy- drocarbon migration and accumulation in the Tertiary Dongying De- pression, Bohai Basin, China 显示文摘 | Carolyn Lampe Guoqi Song Liangzi Cong | 2012 | AAPG2012，96，6： | 1 |
| 20 | Fault control on hydrocarbon migration and accumulation in the Tertiary Dongying Depression,Bohai Basin,China显示文摘 | Carolyn Lampe Guoqi Song Liangzi Cong | 2012 | AAPG Bulletin2012，96，6： | 1 |
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