Tectonics in the northwestern West Philippine basin

The West Philippine basin (WPB) is a currently inactive marginal basin belonging to Philippine Sea plate, which has a complex formation history and various crust structures. Based on gravity, magnetic and seismic data, the tectonics in West Philippine basin is characterized by amagma spreading stage and strike slip fractures. NNE trending Okinawa-Luzon fracture zone is a large fracture zone with apparent geomorphology and shows a right-handed movement. The results of joint gravity-magnetic-seismic inversion suggest that the Okinawa-Luzon fracture zone has intensive deformation and is a transform fault. Western existence of the NW trending fractures under Ryukyu Islands Arc is the main cause of the differences between south and north Okinawa Trough. The Urdaneta plateau is not a remained arc, but remnant of mantle plume although its lava chemistry is similar to oceanic island basalt (OIB).

The characteristics of BSRs and their derived heat flow on the profile 973 in the northeastern South China Sea

Processing of a recently acquired seismic line in the northeastern South China Sea by Project 973 has been conducted to study the character and the distribution of gas hydrate Bottom-Simulating Reflectors (BSRs) in the Hengchun ridge. Analysis of different-type seismic profiles shows that the distribution of BSRs can be revealed to some extents by single-channel profile in this area, but seismic data processing plays an important role to resolve the full distribution of BSRs in this area. BSR' s in the northeastern South China Sea have the typical characteristics of BSRs on worldwide continental margins: they cross sediment bed reflections, they are generally parallel to the seafloor and the associated reflections have strong amplitude and a negative polarity. The characteristics of BSRs in this area are obvious and the BSRs indicate the occurrence of gas hydrate-bearing sediments in the northeastern South China Sea. The depth of the base of the gas-hydrate stability zone was calculated using the phase stability boundary curve of methane hydrate and gas hydrate with mixture gas composition and compared with the observed BSR depth. If a single gradient geothermal curve is used for the calculation, the base of the stability zone for methane hydrate or gas hydrate with a gas mixture composition does not correspond to the depth of the BSRs observed along the whole seismic profile. The geothermal gradient therefore changes significantly along the profile. The geothermal gradient and heat flow were estimated from the BSR data and the calculations show that the geothermal gradient and heat flow decrease from west to east, with the increase of the distance from the trench and the decrease of the distance to the island arc. The calculated 2 heat flow changes from 28 to 64 mW/m(2), which is basically consistent with the measured heat flow in southwestern offshore Taiwan.

Low-amplitude BSRs and gas hydrate concentration on the northern margin of the South China Sea

The passive northern continental margin of the South China Sea is rich in gas hydrates, as inferred from the occurrence of bottom-simulating reflectors (BSR) and from well logging data at Ocean Drilling Program (ODP) drill sites. Nonetheless, BSRs on new 2D multichannel seismic reflection data from the area around the Dongsha Islands (the Dongsha Rise) are not ubiquitous. They are confined to complex diapiric structures and active fault zones located between the Dongsha Rise and the surrounding depressions, implying that gas hydrate occurrence is likewise limited to these areas. Most of the BSRs have low amplitude and are therefore not clearly recognizable. Acoustic impedance provides information on rock properties and has been used to estimate gas hydrate concentration. Gas hydrate-bearing sediments have acoustic impedance that is higher than that of the surrounding sediments devoid of hydrates. Based on well logging data, the relationship between acoustic impedance and porosity can be obtained by a linear regression, and the degree of gas hydrate saturation can be determined using Archie's equation. By applying these methods to multichannel seismic data and well logging data from the northern South China Sea, the gas hydrate concentration is found to be 3-25% of the pore space at ODP Site 1148 depending on sub-surface depth, and is estimated to be less than values of 5% estimated along seismic profile 0101. Our results suggest that saturation of gas hydrate in the northern South China Sea is higher than that estimated from well resistivity log data in the gas hydrate stability zone, but that free gas is scarce beneath this zone. It is probably the scarcity of free gas that is responsible for the low amplitudes of the BSRs.

Polygonal faults and their implications for hydrocarbon reservoirs in the southern Qiongdongnan Basin, South China Sea

The Polygonal faults were identified in Qiongdongnan Basin, South China Sea, by using the technique of time coherent slice and horizon flattening of high-resolution 3D seismic data. These polygonal faults occur in three tiers of the upper Meishan Formation and the Huangliu Formation. The faults have lengths of 150-1500 m, spacings of 50-3000 m, throws of 10-40 m and dips of 50-90 degrees. Tectonic evolution in the Qiongdongnan Basin can be divided into a rifted stage and a post-rifted stage. Tectonic faults are widely distributed in the rifted sequences, but are not well developed in the post-rifted stage. Few faults in the post-rifted sequences might suggest the absence of a migration pathway for hydrocarbon or other fluids. However, the existence of polygonal faults in the post-rifted sequences can serve as the pathway and promote the hydrocarbon migration and accumulation in the Qiongdongnan Basin during the post-rifted stage. (C) 2010 Elsevier Ltd. All rights reserved.

The characteristics of fluid potential in mud diapirs associated with gas hydrates in the Okinawa Trough

Many mud diapirs have been identified in the southern Okinawa Trough from a seismic survey using R/V KEXUE I in 2001. The movement and accumulation of free gas related to mud diapirs are discussed in detail by an analysis of fluid potential which is based upon velocity data. It can be found that free gas moves from the higher fluid potential strata to the lower ones and the gas hydrate comes into being during free gas movement meeting the proper criteria of temperature and pressure. In fact, gas hydrates have been found in the upper layers above the mud diapirs and in host rocks exhibiting other geophysical characteristics. As the result of the formation of the gas hydrate, the free gas bearing strata are enclosed by the gas hydrate bearing strata. Due to the high pressure anomalies of the free gas bearing strata the fluid potential increases noticeably. It can then be concluded that the high fluid potential anomaly on the low fluid potential background may be caused by the presence of the free gas below the gas hydrate bearing strata.

Bottom simulating reflector and gas seepage in Okinawa Trough: Evidence of gas hydrate in an active back-arc basin

To look for gas hydrate, 22 multi-channel and 3 single-channel seismic lines on the East China Sea (ECS) shelf slope and at the bottom of the Okinawa Trough were examined. It was found that there was indeed bottom simulating reflector (BSR) occurrence, but it is very rare. Besides several BSRs, a gas seepage was also found. As shown by the data, both the BSR and gas seepage are all related with local geological structures, such as mud diapir, anticline, and fault-controlled graben-like structure. However, similar structural "anomalies" are quite common in the tectonically very active Okinawa Trough region, but very few of them have developed BSR or gas seepage. The article points out that the main reason is probably the low concentration of organic carbon of the sediment in this area. It was speculated that the rare occurrence of gas hydrates in this region is governed by structure-controlled fluid flow. Numerous faults and fractures form a network of high-permeability channels in the sediment and highly fractured igneous basement to allow fluid circulation and ventilation. Fluid flow in this tectonic environment is driven primarily by thermal buoyancy and takes place on a wide range of spatial scales. The fluid flow may play two roles to facilitate hydrate formation: to help gather enough methane into a small area and to modulate the thermal regime.

Balanced cross section for restoration of tectonic evolution in the southwest Okinawa Trough

On the basis of the multi-channel seismic data and the other data, using 2DMove software, the tectonic evolution in three seismic profiles was restored since Pliocene. The tectonic restoration results show that: (1) the initial active center lay in the west slope and then was transferred to east and south via trough center during the evolution process; (2) several main normal faults controlled the evolution of the southern Okinawa Trough; (3) since Late Pliocene, the southern Okinawa Trough has experienced two spreading stages. The early is depression in Early-Middle Pleistocene and the late is back-are spreading in Late Pleistocene and Holocene, which is in primary oceanic crust spreading stage.

Geophysical evaluation methods for buried hill reservoirs in the Jiyang superdepression of the Bohai Bay basin, eastern China

The Jiyang superdepression is one of the richest hydrocarbon accumulations in the Bohai Bay basin, eastern China. Comprehensive seismic methods have been used in buried hill exploration in Jiyang to describe these fractured reservoirs better. Accurate seismic stratigraphic demarcation and variable-velocity mapping were applied to reveal the inner structure of the buried hills and determine the nature of the structural traps more precisely. Based on the analysis of rock properties and the characteristics of well-developed buried hill reservoirs, we have successfully linked the geology and seismic response by applying seismic forward technology. Log-constrained inversion, absorption coefficient analysis and tectonic forward-inversion with FMI loggings were applied to analyse and evaluate the buried hill reservoirs and gave satisfying results. The reservoir prediction was successful, which confirmed that the comprehensive utilization of these methods can be helpful in the exploration of buried hill reservoirs.

Rifting process and formation mechanisms of syn-rift stage prolongation in the deepwater basin, northern South China Sea

Based on the latest seismic and geological data, tectonic subsidence of three seismic lines in the deepwater area of Pearl River Mouth Basin (PRMB), the northern South China Sea (SCS), is calculated. The result shows that the rifting process of study area is different from the typical passive continental margin basin. Although the seafloor spreading of SCS initiated at 32 Ma, the tectonic subsidence rate does not decrease but increases instead, and then decreases at about 23 Ma, which indicates that the rifting continued after the onset of seafloor spreading until about 23 Ma. The formation thickness exhibits the same phenomenon, that is the syn-rift stage prolonged and the post-rift thermal subsidence delayed. The formation mechanisms are supposed to be three: (1) the lithospheric rigidity of the northern SCS is weak and its ductility is relatively strong, which delayed the strain relaxation resulting from the seafloor spreading; (2) the differential layered independent extension of the lithosphere may be one reason for the delay of post-rift stage; and (3) the southward transition of SCS spreading ridge during 24 to 21 Ma and the corresponding acceleration of seafloor spreading rate then triggered the initiation of large-scale thermal subsidence in the study area at about 23 Ma.

基于正演方法的井间地震响应特征研究

地震勘探的基本任务是测量由人工震源激发的各种地震波，通过对所得到的地震波场的数据记录进行必要的处理和解释而提取所需要的地质信息。不同的地震波场特征反应了不同的地质构造等信息，因此，对地震波场特征进行研究就显得非常重要。井间地震是在一口井中激发、另一口井中接收的一种特殊的地震勘探方法，其实际记录要比常规的地震记录复杂的多，其波场中的各种波也更丰富复杂，如何识别不同类型的波并研究它们的响应特征是一个非常必要的任务。正演模拟可以为地震数据采集、处理、解释提供理论依据，是井间地震波场特征分析的一种有效方法。 本文主要研究了井间地震的数值正演模拟问题，系统地介绍了射线追踪正演模拟和波动方程正演模拟方法，利用Visual Basic 6.0语言编写了相应的射线追踪正演模拟程序，而且分两种方法详细分析了井间地震数值模型的地震响应特征，为直观的井间地震波场识别和勘探地震数据反演提供了必要的依据。本文取得的主要成果如下： 1)在前人的VSP正演模拟的基础上，改进并总结出了一套井间地震射线追踪正演模型的制作方法。 2)编制了井间地震射线追踪正演模拟程序V1.0。 3)利用编写的井间地震正演模拟程序，作了两种射线追踪数值模拟试算；利用Tesseral声波方程正演模拟试算了含有楔形体和丘状体的理论模型；取得了较好的模拟数据。

黄河口地区过渡带地震采集技术研究

环渤海湾海陆过渡带地区有着丰富的油气资源，但过渡带地区具有复杂地表和表层结构，特别是黄河口地区受泥沙影响严重，地震勘探技术受到较大限制，地震资料质量较差。本文针对该区勘探难点，开展过渡带地震波激发震源、检波器耦合、观测系统优化设计、精确定位等技术研究，重点解决滩涂带的激发和接收问题，保证检波器能真实地记录地表的振动，正确记录来自地下的地震反射信号，提高地震信号品质,并保证地震数据有效迭加。 围绕提高滩海过渡带地区地震勘探精度开展研究。在提高淤泥带检波器耦合方面，根据滩海过渡带地区的地震环境和地表结构，设计出不同类型的检波器耦合装置，增加了检波器与淤泥带地表的耦合，保证了检波器真实地记录地表振动，提高了勘探精度。通过多种方法联合应用，形成一套近地表结构精细调查及建模方法，获得了从陆地-过渡带-极浅海连续的高精度表层结构数据。并根据近地表结构模型，指导优选激发参数，形成高效耦合激发技术，提高地震波的主频和信噪比。针对水中检波器随潮水不断漂移而影响同相叠加难点，进行水中检波器的高精度定位技术研究，形成了初至定位和声纳定位联合定位的检波器高精度定位技术，提高地震资料叠加质量。通过研究炸药爆炸理论，优化延迟叠加震源参数，拓宽地震子波的频带，提高了地震资料的信噪比，减小了与气枪震源之间的差异。针对提高过渡带地震采集资料信噪比，提出了从地震波激发、地震波接收以及观测系统设计环节综合压噪方法。通过应用以上技术，滩海过渡带地震资料的信噪比和分辨率较老资料有明显的提高，取得了较好的勘探效果。

皱纹盘鲍血细胞内活性氧抗病机制及几种环境污染物及其影响的研究

本研究首次揭示了皱纹盘鲍(Haliotis discus hannai) 血细胞内存在着利用活性氧（Reactive oxygen species, ROS）的抗病机制。为今后我国研究贝类的活性氧抗病机制和筛选免疫药物提供了理论基础。本研究主要结果如下：1. 利用鲁米诺（Luminol, 3-氨基邻苯二甲酰肼）为依赖的化学发光法在体外条件下用不同刺激物（酵母细胞和酵母聚糖）对皱纹盘鲍血细胞进行刺激，测定血细胞吞噬活动中历经呼吸爆发产生活性氧的化学发光反应。结果表明皱纹盘鲍血细胞在体外条件下，经刺激物诱导吞噬活动中有明显的呼吸爆现象和很强的活性氧产生。不同有刺激物诱导血细胞产生的化学发光强度不同；同一刺激物的不同处理和不同浓度对血细胞产生活性氧的化学发光强度的影响不同。刺激物经皱纹盘鲍自体血清调理和未经调理对血细胞刺激所产生的化学发光强度不同。SOD和NaN_3对皱纹盘鲍血细胞吞噬过程中活性氧产生的化学发光有抑制作用。上述结果证明了皱纹盘鲍血细胞内存在有象高等动物血细胞内一样的MPO-H_2O-卤素系统的氧化性抗病机制，即在血细胞吞噬异物过程中能够释放活性氧（ROS）对异物进行杀灭的功能。2. 利用活性氧清除剂（过氧化氢酶、SOD、苯甲酸钠、2，5-二甲基呋喃、NBT和EDTA等）对皱纹盘鲍血细胞释放的活性氧进行分类测试，结果表明活性氧清除剂对皱纹盘鲍血细胞吞噬的化学发光都有明显的抑制作用，从而证明皱纹盘鲍血细胞能够释放的活性氧的种类有：超氧阴离子（O_2~-），过氧化氢（H_2O_2），羟自由基（OH~·）和单线态氧（~1O_2）。3. 在体外条件下利用化学发光法定量地研究了不同种类和不同浓度的农药：对硫磷（Parathion）、敌敌畏（Dichlorovos)、乐果（Dimethoate)、2，4-D 丁酯(2,4-D butylester)和甲胺磷（Methamidophos）对皱纹盘鲍血细胞氧化性抗病机制的影响。结果显示不同农药对皱纹鲍血细胞产生ROS的影响程度不同，及同一种农药的不同浓度的浸泡1h或浸泡12h处理皱纹盘鲍血细胞都能够抑制血细胞吞噬时的化学发光，表明农药能够抑制皱纹敌国鲍血细胞吞噬活动中的活性氧（ROS）的产生，而且这种抑制作用随着农药浓度的增加而加强。几种农药抑制皱纹盘鲍血细胞产生活性氧（ROS）的强度不同：2，4D-丁酯，敌敌畏和乐果的抑制作用强于对硫磷和甲胺磷。同时测定了不同浓度的农药浸泡12h后的皱纹盘鲍因细胞吞噬酵母细胞的吞噬百分率和吞噬指数，结果显示多数农药在低浓度时能够提高皱纹盘鲍血细胞的吞噬百分率和吞噬指数，而在高浓度时则能抑制血细胞吞噬酵母细胞的活力而降低血细胞的吞噬百分率的吞噬指数。4. 在体外条件下利用化学发光法定量地研究了不同种类和不同浓度的重金属：铭（Cr）、镉（Cd）、汞（Hg）、铅（Pb）、铜（Cu）和锌（Zn）对皱纹盘鲍血细胞氧化性抗病机制的影响。结果显示不同种类和不同浓度的重金属浸泡1hr.处理皱纹盘鲍血细胞都不同程度地抑制了血细胞吞噬时的化学发光，表明重金属能够抑制皱纹盘鲍血细胞吞噬活动中的活性氧（ROS）的产生，而且这种抑制作用随着重金属浓度的增加而加强。不同的重金属抑制强度不同，从强到弱依次为Hg > Cd > Cu > Pb > Cr > Zn. 研究表明六种重金属中，Hg对皱纹盘鲍血细胞的免疫毒性最大。

渤海湾盆地济阳坳陷东部走滑构造特征及其对油气成藏的影响研究

研究区位于郯庐断裂中段与济阳坳陷的构造结合部，区内走滑构造广泛发育，主要的走滑断裂有7条，分别是郯庐断裂带的东西两支、垦东断层、孤东断层、长堤断层、埕东断层和发育于垦东凸起中部的浅层走滑构造带。走滑构造带与油气富集带有着明显的对应关系。 通过对研究区内二维、三维地震测线和平面构造图的精细解释和分析，分别揭示了各走滑断裂在平面、剖面和三维空间上的构造形态。根据走滑断裂及其伴生构造的平面和剖面上的几何学特征，将研究区内的走滑断裂划分为三种类型：成熟型走滑断裂、隐伏型走滑断裂、不连续型的走滑断裂。 从理论模式研究入手，推导了拉分盆地中盆地的走滑速率与沉降速率之间的关系，证实了走滑速率同盆地的几何形状参数、最大沉降深度和盆地的沉降速率存在着稳定的数值关系。通过对莱州湾地区潍北凹陷基底沉降历史的分析，建立了潍北凹陷沉降速率与郯庐断裂中段走滑速率之间的经验关系式，进而求出郯庐断裂中段新生代右行走滑位移量的大小为40km。 运用2DMove软件，对研究区内四条典型剖面进行构造复原，计算出了各条剖面每个时期的伸展参数，对研究区构造活动强度进行了定量分析，揭示了研究区的构造演化规律。通过运用Ansys软件进行有限元模拟，恢复了晚白垩世晚期-古近纪早期研究区内的构造应力场和应变场，揭示了扭张作用是研究区内走滑断层开始走滑的主要原因。 通过上述分析，结合对究区内近几年勘探开发成功和失败的实例分析，全面探讨了走滑活动对于油气成藏“生”、“储”、“盖”、“圈”、“运”、“保”各因素的影响。

肉食性鱼类补偿生长特性的研究

本文主要以花鲈[Lateolabrax．japonicus (C．& V．)]和褐牙鲆[Paralichthys olivaceus(T. & S.)]作为海洋肉食性鱼类的代表种类，根据鱼类生态生理学理论，通过设定不同饥饿时问下因子水平，研究两种鱼类摄食率、排粪率、转化效率和SGR等生态生理效率的状态变化。其目的在于研究高营养级鱼类在海洋生态系统中的下行控制作用(Top-down Effect)，以及肉食性鱼类的生态对策与鱼类资源补充机制的相互关系，为深入解析鱼类资源生产力及其持续利用海洋生物资源，提供科学依据。其主要研究结果概述如下：1．花鲈： 饥饿0(对照组)、4、8、12、16d后恢复投喂，过量投喂淡水桡足类，温度为19.5±2.0℃，初始体重为0.61-0.93g，平均体重为0．79g实验周期为28d。1.1饥饿时间对花鲈的体重损失率产生显著影响，受过饥饿的个体的湿重失率 (LR_W)与饥饿时间(t)的关系为：LR_W=2.2164t-3.6634(r~2=0.9767，p13d)的个体的排粪率显著大于其它各组，其它各组间排粪率差异不显著；2.2在整个实验周期36d内，对照组与经受3—8d饥饿的实验组的SGR显著大于经受饥饿时间大于lOd的实验组，饥饿3-8d的完全补偿生长，饥饿10-15d 的个体发生部分补偿生长，饥饿18d的个体不能补偿生长；经受饥饿个体的摄食率低于对照组；除了饥饿18d的个体的饵料转化率显著小于对照组外，其它各组的转化率没有显著差异；经受长时间饥饿(>13d)的个体的排粪率显著大于其它各组，其它各组问没有显著的差异。2．3平均体重为2．59g的褐牙鲆，饥饿至不可恢复点(PNR)的时间大于18d。3．花鲈和褐牙鲆在经受饥饿后的体重损失率与饥饿的时间正相关。在实验期间，花鲈体重损失率与饥饿时间成一次线性关系，褐牙鲆体重损失率与饥饿时间成对数函数关系。在饥饿后均会发生补偿生长。3.1比较研究结果，表明在适当时间饥饿后的个体均会发生补偿生长，其超生长速度与饥饿时间密切相关。花鲈在饥饿至不可恢复点的临界状态时发生最强烈的超生长现象，而褐牙鲆则是在饥饿3—5d后恢复投喂时可以观测到最高速度的超生长。3.2经受适当时间饥饿后的个体在短期内，其摄食率大于对照组的摄食强度。曾经饥饿的时间越长，花鲈在饥饿结束后的摄食率越高，褐牙鲆在饥饿结束后的高摄食率持续的时间越长。3.3经受适当时间饥饿后的个体，在短期内的转化率均会大于对照组的转化 效率，且随饥饿时间而加强；高转化效率持续的时间与饥饿时间无关。褐牙鲆的高转化率持续的时间很短，且很快下降至低于对照组的水平，其下降程度与饥饿时问成正相关，经受过度饥饿的花鲈和褐牙鲆转化率显著低于对照组。3．4花鲈的补偿生长是饵料转化率提高的结果；而褐牙鲆的补偿生长的原因则因其经受的饥饿程度而异。从饥饿后恢复投喂较短的时间周期(4d和6d)看，花鲈和褐牙鲆的补偿生长是转化率和摄食率共同提高的结果；但从饥饿后恢复投喂较长的时问周期(12d和1 8d)看，经受短期(4-8d)饥饿的花鲈的补偿生长是转化率显著提高的结果，而经受长期(12d)饥饿的花鲈的补偿生长是转化率显著提高的结果，褐牙鲆则是摄食率显著提高的结果。3．5从整个实验周期来看，对花鲈的饥饿降低了其生长速度和饵料转化率，但对褐牙鲆的短期饥饿(<8d)不会降低其生长速度，也不会影响一定时间(3-13d)饥饿的个体的饵料转化率。

南海北部陆缘深水区构造演化及其资源效应

南海北部陆缘深水区（水深>300m）蕴藏着丰富的资源，我国对深水区的地质研究刚刚起步，但相关领域已成为科研热点。深水油气盆地的构造演化是油气勘探中最重要的基础性研究之一，因此针对我国南海北部陆缘深水区开展构造演化及其资源效应的研究具有重要的理论意义和实际意义。 本文利用钻井和地震资料并结合区域地质资料，重点研究了珠江口盆地深水区的结构和构造演化，取得如下创新性成果：1）首次利用半地堑分析方法系统解剖了研究区的结构、各构造单元发育特征，在此基础上指出五个有利油气运聚带；2）采用回剥法并利用最新资料进行校正，得到了研究区更为可靠的构造沉降曲线，重新划分了裂陷期和裂后期的分界，认为32Ma南海海底扩张之后裂陷作用仍在持续，直到23Ma左右才开始大规模裂后热沉降，并进一步解释了裂陷期延迟的形成机制；3）应用非连续拉张模型计算拉张系数的方程计算了研究区的壳幔拉张系数，指出了深水区地幔相对于地壳的优势伸展作用；首次运用平衡剖面技术重建了研究区的构造发育史，计算了各构造期的拉张率和沉积速率，指出研究区新生代整体呈现持续拉张，拉张系数在1.1-1.24之间；4）精细刻画了水合物钻采区的地质构造特征，建立了该区天然气水合物成藏的概念模式；建立了一套根据地震叠加速度计算流体势的方法，为水合物成藏规律的研究提供了新的思路。