首页> 外文会议>Annual Indonesian Petroleum Association convention and exhibition;Indonesian Petroleum Association convention and exhibition;IPA >SURFACE GEOCHEMICAL EXPLORATION AND HEAT FLOW SURVEYS IN FIFTEEN (15) FRONTIER INDONESIAN BASINS
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SURFACE GEOCHEMICAL EXPLORATION AND HEAT FLOW SURVEYS IN FIFTEEN (15) FRONTIER INDONESIAN BASINS

机译:十五个印尼前盆地的地表地球化学勘查和热流调查

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TDI-Brooks International, Inc., under contract to TGS-NOPEC, conducted an extensive Surface Geochemical Exploration (SGE) survey in 15 frontier basins in Indonesia between April 2007 and March 2008. The Indonesian Frontier Basins (IFB) Project is a multidisciplinary program designed to generate meaningful petroleum exploration data throughout Indonesia's under-explored frontier basins. The SGE program was the final step in this study designed to evaluate hydrocarbon charge in these offshore frontier basins. Core sites were selected based on multibeambathymetry/backscatter anomalies at sites potentially indicative of seepage combined with 2-D seismic data where available to assist in delineating seep conduits from depth to the seafloor. A 1-km long Chirp subbottom profiler line was acquired over each target site to further refine the core position. Sub-bottom profiles were used to adjust some targets toward sites of potential seepage, or used to avoid hardgrounds that would yield little to no recovery as well as damage the core. Approximately 1,400 piston cores were acquired during the study using the TDI-Brooks research vessel R/V GeoExplorer. The 1,000 kg piston core rigs used 3, 6 and 9 m long × 7.5 cm OD barrels, and were positioned with an Ultra-Short Baseline (USBL) navigation system to within 25 m of the pre-selected seabed targets. Core recovery was typically 3 to 8 m of sediment column, although recovery was affected by bottom type. Many sites with carbonate hard-bottom were selected during this program, and core recovery at such sites was sometimes limited to less than 1 m. Three sediment sections per piston core were typically sampled at about 1 m intervals from the bottom of each core todetermine the presence of any thermally sourced hydrocarbons.Analytical screening measurements included: (1) the fluorescence spectra from bagged sediment sections using dried-sediment solvent extraction, (2) the C_(15+) hydrocarbon concentrations by gas chromatography in the same sediment extracts, and (3) the interstitial light hydrocarbon gas concentrations from separately canned sediment sections using wet-sediment gas partitioning and gas chromatography. From these analyses, screening indicators of migrated liquid and gaseous thermogenic hydrocarbons were developed and used to qualify cores and distinguish them from defined background thresholds for this study area.Sediment extracts of this study, each representing one section of a core acquired at a site of interest, were qualified for the unambiguous presence of migrated liquid petroleum (thermogenic) hydrocarbons by the following criteria using background thresholds of: TSF Maximum Intensity ≥ 10,000 and UCM ≥ 10 μg/g, or T/D ≥ 1.5. Using these screening criteria, 118 of the 927 cores (13 percent) exhibited unambiguous evidence of liquid petroleum hydrocarbons. This is an unusually high percentage of oil seep shows for our SGE surveys (compared to about 8 percent on average globally, and <5 percent on average in frontier basins), and attests to the potential of the region as well as to the quality of the targets selected.The concentrations of alkane gases in the canned samples typically increased with depth in a core. The strength of the interstitial gas screening indicators as prospecting tools improved significantly with depth over the 3-8 m range typically retrieved by our method of piston coring. Coring carbonate hard-bottom sites reduced such depth-recovery at many of the sites, but high concentrations of gas were measured at some of these hard-bottom sites. Sediment samples canned for interstitial gas measurements, each representing one section of a cpre acquired at a site of interest, were qualified for the unambiguous presence of migrated thermogenic gases in the following manner: (1) an ethane/ethene ratio of at least unity, and (2) the product of the ethane/ethene ratio and the total alkane gas concentration (in ppmV) being at least 100, in at l
机译:TDI-Brooks International,Inc.根据TGS-NOPEC的合同,于2007年4月至2008年3月在印度尼西亚的15个边境盆地进行了广泛的地表地球化学勘探(SGE)调查。印尼边境盆地(IFB)项目是一项多学科计划旨在为整个印度尼西亚未充分开发的边境盆地生成有意义的石油勘探数据。 SGE计划是这项研究的最后一步,旨在评估这些近海边境盆地的碳氢化合物装量。基于多波束选择核心站点 可能指示渗漏的站点的测深/反向散射异常与二维地震数据相结合,可用于帮助描绘从深度到海底的渗漏管道。在每个目标位置上获取了一条1公里长的Chirp底部轮廓剖面线,以进一步完善核心位置。次底部轮廓用于将一些目标调整到可能的渗漏位置,或者用于避免产生很少甚至没有恢复以及损坏岩心的硬质地面。在研究过程中,使用TDI-Brooks研究船R / V GeoExplorer采集了大约1400个活塞芯。 1,000公斤的活塞核心钻机使用3、6和9 m长×7.5 cm OD桶,并使用超短基线(USBL)导航系统定位在距预先选定的海底目标25 m以内的位置。核心恢复通常为沉积物柱3至8 m,尽管恢复受底部类型的影响。在该程序中选择了许多碳酸盐岩硬底的位置,有时在这些位置的岩心采收率被限制为小于1 m。每个活塞芯的三个沉积物截面通常从每个芯的底部到底部大约1 m的间隔进行采样 确定是否存在任何热源碳氢化合物。 分析筛选测量包括:(1)使用干沉溶剂萃取法从袋装沉积物切片中获得的荧光光谱;(2)通过气相色谱法在相同沉积物萃取物中的C_(15+)烃浓度;以及(3)间隙轻质烃使用湿沉降气体分配和气相色谱仪从单独的罐装沉积物段中收集气体浓度。通过这些分析,开发出了迁移的液态和气态产热烃的筛选指标,并用于限定岩心,并将其与该研究区域的已定义背景阈值区分开。 这项研究的沉积物提取物,每个代表在感兴趣的地点采集的岩心的一部分,根据以下标准使用以下阈值确定了迁移的液态石油(生热)碳氢化合物的明确存在:TSF最大强度≥10,000和UCM ≥10μg/ g,或T / D≥1.5。使用这些筛选标准,在927个岩心中有118个岩心(占13%)显示出液态石油烃的明确证据。对于我们的SGE调查而言,这是石油渗透率的异常高的百分比(相比之下,全球平均水平约为8%,边境盆地平均水平低于5%),并证明了该地区的潜力和质量选择的目标。 罐装样品中烷烃气体的浓度通常随堆芯中的深度而增加。在我们通常采用活塞取芯方法获得的3-8 m范围内的深度范围内,作为勘探工具的间隙气体筛选指示器的强度得到了显着提高。碳酸盐岩硬底位置降低了许多位置的深度恢复能力,但是在其中一些硬底位置测量到了高浓度的气体。罐装用于间隙气体测量的沉积物样品,每个都代表在感兴趣的地点采集的cpre的一部分,以下列方式明确存在迁移热气的明确存在:(1)乙烷/乙烯比至少为1, (2)乙烷/乙烯比与总烷气浓度(ppmV)至少为100的乘积,在1

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