共查询到20条相似文献，搜索用时 546 毫秒
1.
重论"上生下储"与"侧向运移" 总被引：1，自引：0，他引：1
油气运移是油气藏形成与分布研究的基础．随着生油层理论的建立和发展,油气“上生下储”与“侧向运移”已经成为解释生油层与储集层关系的金科玉律．随着世界范围内油气勘探实践的积累和油气形成与分布研究,特别是对基岩油气藏勘探研究的不断深入,上述运移途径需要重新加以认识。 相似文献
2.
Stratum energy of coal-bed gas reservoir, including coal-radix flexibility energy, groundwater flexibility energy and gas flexibility energy (hereinafter "three energy"), depends on the energy homeostasis system, the core process of which is the effective transfer of energy and the geological selective process. Combining with the mechanics experimentations of coal samples, different flexibility energy has been analyzed and researched quantificationally, and a profound discussion to their controls on the coal-bed gas reservoir formation has been made. It is shown that when gas reservoir is surrounded by edge water and bottom water, the deposited energy in the early phase of forming gas reservoir is mostly coal-radix and gas flexibility energy, but the effect of groundwater flexibility energy increases while water-body increases. The deposited energy in the middle and later phase of forming gas reser voir is mostly gas flexibility energy, which is greater than 80% of all deposited energy. In the whole process, larger groundwater body exerts greater influences on gas accumulation. The paper indicated that higher stratum energy is more propitious to forming coal-bed gas reservoir. And higher coal-radix flexibility energy and gas flexibility energy are more propitious to higher yield of gas reservoirs, while higher groundwater flexibility energy is more propitious to stable yield of gas reservoirs. Therefore, the key to evaluating the coal-bed gas reservoir formation is the stratum energy of coal-bed gas reservoir. 相似文献
3.
Natural gas generation model and its response in accumulated fluids in the Yinggehai basin 总被引：2，自引：0，他引：2
The generation of natural gases is much more complicated in comparison with liquid petro-leum in that natural gases could be generated from both humic and sapropelic organic matter at different stages and that natural gases could be organic and inorganic … 相似文献
4.
《中国科学D辑(英文版)》2008,(Z1)
The components and carbon isotope of gases in inclusions are one of the most important geochemical indexes for gas pools.The analysis results of the components and carbon isotope of gases from inclusions in reservoir layers of Upper Palaeozoic gas pools in the Ordos Basin show that most inclusions grown in reservoir sandstone are primary inclusions.There is only a little difference about the components and carbon isotope between the well gases and the secondary inclusions gases.This indicated that the epigenetic change of gas pools is little.This difference between the well gases and the secondary inclusions gases is caused by two reasons:(i)The well gases come from several disconnected sand bodies buried in a segment of depth,while the inclusion gases come from a point of depth.(ii)The secondary inclusions trapped the gases generated in the former stage of source rock gas generation,and the well gases are the mixed gases generated in all the stages.It is irresponsible to reconstruct the palaeo-temperature and palaeo-pressure under which the gas pool formed using carbon dioxide inclusions. 相似文献
5.
JingKui Mi JinXing Dai ShuiChang Zhang WenZheng Zhang Se Gong XianQing Li 《中国科学D辑(英文版)》2008,51(1):115-121
The components and carbon isotope of gases in inclusions are one of the most important geochemical indexes for gas pools. The analysis results of the components and carbon isotope of gases from inclusions in reservoir layers of Upper Palaeozoic gas pools in the Ordos Basin show that most inclusions grown in reservoir sandstone are primary inclusions. There is only a little difference about the components and carbon isotope between the well gases and the secondary inclusions gases. This indicated that the epigenetic change of gas pools is little. This difference between the well gases and the secondary inclusions gases is caused by two reasons: (i) The well gases come from several disconnected sand bodies buried in a segment of depth, while the inclusion gases come from a point of depth. (ii) The secondary inclusions trapped the gases generated in the former stage of source rock gas generation, and the well gases are the mixed gases generated in all the stages. It is irresponsible to reconstruct the palaeo-temperature and palaeo-pressure under which the gas pool formed using carbon dioxide inclusions. 相似文献
6.
Mi JingKui Dai JinXing Zhang ShuiChang Zhang WenZheng Gong Se Li XianQing 《中国科学:地球科学(英文版)》2008,51(1):115-121
The components and carbon isotope of gases in inclusions are one of the most important geochemical indexes for gas pools. The analysis results of the components and carbon isotope of gases from inclusions in reservoir layers of Upper Palaeozoic gas pools in the Ordos Basin show that most inclusions grown in reservoir sandstone are primary inclusions. There is only a little difference about the components and carbon isotope between the well gases and the secondary inclusions gases. This indicated that the epigenetic change of gas pools is little. This difference between the well gases and the secondary inclusions gases is caused by two reasons: (i) The well gases come from several disconnected sand bodies buried in a segment of depth, while the inclusion gases come from a point of depth. (ii) The secondary inclusions trapped the gases generated in the former stage of source rock gas generation, and the well gases are the mixed gases generated in all the stages. It is irresponsible to reconstruct the palaeo-temperature and palaeo-pressure under which the gas pool formed using carbon dioxide inclusions.
相似文献7.
南海含天然气水合物地层地震反射特征及可能分布研究 总被引：4，自引：0，他引：4
天然气水合物是当前能源与环境领域的研究热点之一,南中国海是天然气水合物赋存的有利区域。天然气水合物的存在改变了沉积地层的声学特征,这一性质使多道地震勘探成为发现海洋天然气水合物的主要手段。本文首先根据地震成像结果定性分析南海可能含天然气水合物沉积地层的地震反射特征,初步确定天然气水合物存在的可能性并指出地震成像关键技术。在无井条件下,构建虚拟井进行波阻抗反演得到定量的地层速度参数进一步证实这一可能性,最后将反演获得的速度场与ODP184 航次在此区域获得的地球物理、地球化学信息综合分析,可以确定此区域天然气水合物的存在及其空间展布。 相似文献
8.
Geological analysis and physical modeling of structural pumping in high effective formation of Kela 2 gas field 总被引：1，自引：1，他引：1
In a 3-D closed geological body, in case “structural expanding” inside is induced by stress, it can produce the pressure difference between the expanding cell and surrounding rock, then generate a pumping force directed toward the cell and accelerate the directional flow of fluid in the strata. The structural style and conditions of gas reservoir-formation in the Kuqa depression are favorable to the structural pumping. According to similarity principle, a physical modeling of structure formation and gas filling process of the Kela 2 gas field has justified the occurrence of structural pumping and its important role in gas-reservoir formation with high efficiency under the compressive and well-sealed circumstance. Therefore, authors propose that structural pumping is an important mechanism of gas reservoir-formation with high efficiency in the Kuqa depression. 相似文献
9.
10.
南海北部陆坡包括神狐海域在内无论在横向上还是纵向上影响水合物形成与分布的地质因素差异较大,其气源条件的变化是否为一种重要因素值得探索.本文将前人南海北部陆坡气源类型和气体组成概括为14种情况,分别运用模拟手段定量-半定量地分析它们对水合物成藏可能带来的影响.模拟结果显示,与神狐海域已知水合物相比,不同气体组成形成水合物所需温度条件增大0.49~5.44℃,多数增大2℃以上.可以看出,不同气体组成明显改变水合物的形成条件,暗示着不同类型气源可能是影响南海北部陆坡水合物形成与分布的重要因素. 相似文献
11.
Douglas M. Thompson 《地球表面变化过程与地形》2001,26(11):1195-1212
Average pool spacing between five and seven bankfull widths has been documented in environments throughout the world, but has limited theoretical justification in coarse‐bedded and bedrock environments. Pool formation in coarse‐bedded and bedrock channels has been attributed to bedrock and boulder constrictions. Because the spacing of these constrictions may be irregular in nature, it is difficult to reconcile pool‐formation processes with the supposedly rhythmic spacing of pools and riffles. To address these issues, a simulation model for pool and riffle formation is used to demonstrate that semi‐rhythmic spacing of pools with an approximate spacing of five to seven bankfull widths can be recreated from a random distribution of obstructions and minimum pool‐ and riffle‐length criteria. It is assumed that a pool–riffle couplet will achieve a minimum length based on dominant‐discharge conditions. Values for the minimum‐length assumption are based on field data collected in New England and California, while the theoretical basis relies on the demonstrated hydraulic response of individual pools to elongation. Results from the simulations show that the location of pools can be primarily random in character, but still assume an average spacing between four and eight bankfull widths for a variety of conditions. Field verification data generally support the model but highlight a highly skewed distribution of pool‐forming elements and pool spacing. The relation between pool spacing and bankfull widths is attributed to the common geometric response of these features to dominant‐discharge conditions. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
12.
13.
A direct detection of hydrocarbons is used by connecting increased attenuation of seismic waves with oil and gas fields. This study analyzes the seismic attenuation of P- and S-waves in one tight sandstone gas reservoir and attempts to give the quantitative distinguishing results of gas and water by the characteristics of the seismic attenuation of P- and S-waves. The Hilbert–Huang Transform (HHT) is used to better measure attenuation associated with gas saturation. A formation absorption section is defined to compute the values of attenuation using the common frequency sections obtained by the HHT method. Values of attenuation have been extracted from three seismic sections intersecting three different wells: one gas-saturated well, one fully water-saturated well, and one gas- and water- saturated well. For the seismic data from the Sulige gas field located in northwest Ordos Basin, China, we observed that in the gas-saturated media the S-wave attenuation was very low and much lower than the P-wave attenuation. In the fully water-saturated media the S-wave attenuation was higher than the P-wave attenuation. We suggest that the joint application of P- and S-wave attenuation can improve the direct detection between gas and water in seismic sections. This study is hoped to be useful in seismic exploration as an aid for distinguishing gas and water from gas- and water-bearing formations. 相似文献
14.
The causes of the formation of neutral gas temperature and density equatorial minimums on the dayside, recently detected from
satellite measurements, have been studied based on a global numerical model of the Earth’s upper atmosphere (UAM). The performed
numerical experiments made it possible to conclude that these minimums are not related to the magnetospheric sources of energy
and momentum and electric fields of the dynamo origin. It has been indicated that the absorbed solar ionizing radiation and
rotation of the Earth are responsible for the formation of the neutral gas temperature and density equatorial minimums on
the dayside. 相似文献
15.
Peng Weilong Liu Quanyou Zhang Ying Jia Huichong Zhu Dongya Meng Qingqiang Wu Xiaoqi Deng Shang Ma Yongsheng 《中国科学:地球科学(英文版)》2022,65(5):874-881
Science China Earth Sciences - Helium gas is a scarce but important strategic resource, which is usually associated with natural gas. Presently, only one extra-large helium-rich gas field has been... 相似文献
16.
人工诱发地震现象已经有很久的历史.水库蓄水、采矿、地热开发、从地下提取液体或气体,或将液体注入地球内部都可能诱发地震.大量地震监测数据与科学分析结果显示:美国俄克拉何马州的地震剧增主要与页岩油气开采的废水回注量相关;加拿大阿尔伯塔省的地震剧增主要与页岩油气开采水力压裂的工作量相关;而荷兰罗宁根天然气田的传统天然气开采也同样诱发了较强的地震活动.在中国四川盆地的页岩油气开发区域,地震活动近几年也大幅度增强,但目前监测与科研工作较少,对某些地震成因尚有争议.目前研究诱发地震问题已成为学术界与工业界的一门专业学科.推断诱发地震,除了分析时空分布与工业活动的相关性之外,本文综述了该领域基于地震学、地质动力学、构造地质学的多种分析方法.如何在油气开采过程中减少诱发地震的灾害影响成为当前相关各界极为关注的科研问题,本文介绍了多个国家或地区建立的控制诱发地震的管理系统、基于地震大数据的诱发地震概率预测方法,以及基于地球物理与地质信息的综合诱发地震风险评估方法,并对我国控制诱发地震问题提出建设性意见. 相似文献
17.
Commercial accumulation of mantle-derived helium in the sedimentary shell is discussed. Generally speaking, a commercial helium
pool is formed by accumulated4He that comes from uranium and thorium via α-decay; therefore, it has a very low3He/4He value in the magnitude of 10-8. The helium concentration in some gas wells of eastern China oil/gas provinces is about or over 0.05% —0. 1%, consequently
forming commercial helium wells (pools), such as the Wangjinta Gas Pool in Songliao Basin, Huangqiao Gas Pool in North Jiangsu
Basin and some gas wells in Sanshui Basin. Studies have proved that when the3He/4He value of a helium gas pool is about 3.7 × 10-6 -7.2×10-6 namely mantle-derived helium in its total helium concentration accounts for 33.5%—65.4%, it is a crust-mantle dual-source
or dominantly mantle-derived helium gas pool, which is a novel helium resource and its formation is mainly related to the
distribution of megafractures. 相似文献
18.
The Dongfang 13-1 is located in the diapiric structure belt of the Yinggehai Basin. The formation pressure of its main gas reservoir in the Miocene Huangliu Formation is up to 54.6 MPa(pressure coefficient=1.91) and the temperature is as high as 143°C(geothermal gradient 4.36°C/100 m), indicating that it is a typical high-temperature and overpressured gas reservoir. The natural gas is interpreted to be coal-type gas derived from the Miocene mature source rocks containing type II2-III kerogens as evidenced by high dryness index of up to 0.98 and heavy carbon isotopes, i.e., the δ13C1 ranging from -30.76‰ to -37.52‰ and δ13C2 ranging from -25.02‰ to -25.62‰. The high temperature and overpressured Miocene petroleum system is related mainly to diapir in the Yinggehai Basin and contains more pore water in the overpressured reservoirs due to undercompaction process. The experimental and calculated results show that the solubility of natural gas in formation water is as high as 10.5 m3/m3 under the temperature and pressure conditions of the Sanya Formation, indicating that at least part of the gas may migrate in the form of water-soluble phase. Meanwhile, the abundant gas source in the Basin makes it possible for the rapid saturation of natural gas in formation water and exsolution of soluble gas. Therefore, the main elements controlling formation of the Dongfang 13-1 gas pool include that(1) the diapir activities and accompanying changes in temperature and pressure accelerate the water-soluble gas exsolution and release a lot of free gas;(2) submarine fan fine sandstone in the Huangliu Formation provides good gas-water segregation and accumulation space; and(3) the overlying overpressured mud rocks act as effective caps. The accumulation mechanism reveals that the high temperatural and high pressure structure belt near the diapir structures has a good potential for large and medium-sized gas field exploration. 相似文献
19.
WANG Tingbin Exploration Production Research Institute SINOPEC Beijing China 《中国科学D辑(英文版)》2005,48(4):454-466
Coal is the richest fossil fuel in the world. Theby-product formed during incoalation is gas that iscomposed primarily of methane (CH4)[1,2]. This gascan generally be named coal measure gas. Accordingto the occurrence conditions, coal measure gas can befurther divided into humic gas and coal-bed methane.Humic gas refers to coal measure gas that generatesfrom the coal measure source rocks (coal and dark-coloured argillaceous rocks in coal measures), and canbe expelled and migrate into various … 相似文献
20.
Tectonic and geochemical characteristics and reserved conditions of a mantle source gas accumulation zone in eastern China 总被引：8，自引：0，他引：8
Along both sides of the Tancheng-Lujiang Fracture Zone in eastern China, a series of mantle source gas pools constitute a
massive-scale tectonic accumulation zone in NNE direction, with the mantle geochemical characteristics of high concentrations
of C02 and He, high3He/4He-40Ar/36Ar ratio system and high δ13Coo2 ratios (the main frequency, -3.4%— 4.6%), showing no difference from the tectonic framework of the area. In the area, the
tectonic environment is a rift formed as a result of diapiric mantle injection and crust thinning to form graben-type basins
and lithospheric fractures. The mantle-derived volcanic rocks and inclusions are well-developed and a high geothermal zone
(mantlesource) exists in the area. The characteristics of the three components (solid, liquid and gas) of mantle, concentrated
all over the same tectonic space zone, show that the rift system is of a good tectonic environment or passage for mantle degassing
and gas migration. The main types of the gas pools are volcano, fault-block, anticline, buried hill and so on, but most of
them are combination traps closely related with fracture. For the mantle source gas pools, rift is an optimum tectonic region,
and nearby lithospheric fracture, mantle source volcanic rocks or basement uplifts are a favourable structural location when
reservoir-caprock association develops. 相似文献