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The geology of offshore drilling through basalt sequences: Understanding operational complications to improve efficiency

机译:通过玄武岩层序进行海上钻井的地质学:了解操作复杂性以提高效率

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Offshore drilling in basins with a significant basaltic component poses a number of complications to drilling operations. These include slow and variable rates of penetration (ROP), drilling fluid losses, drill bit or string sticking, overpressured formations, wellbore spatting and collapse. In this contribution we investigate features of large igneous province (LIP). volcanic facies that may directly contribute to drilling complications. Combining borehole and field based examples we identify highly vesicular brecciated lava flow tops and hydro-volcanic facies as a major potential cause of catastrophic drilling fluid losses. The risk for drilling losses is generally higher in the upper parts of thick volcanic successions where hydrothermal secondary mineralization and alteration may be less pervasive. We demonstrate how these fades may be identified early by integrating real time mud logging data with characteristic drill cuttings and LWD (logging while drilling) wireline data as it becomes available. We highlight the potential of basaltic formations to maintain porosity and permeability to greater depths than is typical for sediments due to the high compressive strength of crystalline basalt frameworks. The heterogeneous sub surface distribution of key volcanic facies commonly includes intimate mixing and layering of hard and dense with soft and weak volcanic rock which may promote complex in-situ stresses to develop during burial compaction. Where this occurs, wellbore stability predictions such as the fracture and wellbore collapse gradients for volcanic sequences may deviate from those expected in basin equivalent sedimentary sequences. Examples of swelling volcanic clay horizons, unstable volcaniclastic sequences, and intrusion related ledge effects are used to characterize the main causes of drill bit and string sticking. A greater understanding of drilling complications encountered within prospective areas containing volcanic sequences is needed if better pre-drilling risk assessment, cost prediction, real-time identification and mitigation is to be achieved. (C) 2016 Elsevier Ltd. All rights reserved.
机译:玄武岩成分丰富的盆地中的海上钻井给钻井作业带来了许多麻烦。这些包括缓慢的和可变的渗透率(ROP),钻井液流失,钻头或钻柱卡死,超压地层,井眼崩裂和塌陷。在本文中,我们研究了大火成岩省(LIP)的特征。可能直接导致钻井复杂化的火山岩相。结合基于钻孔和野外的实例,我们确定高泡角砾化的熔岩流顶部和水汽相是造成灾难性钻井液损失的主要潜在原因。在热液次生矿化和蚀变较不普遍的厚火山演替层的上部,钻井损失的风险通常较高。我们演示了如何通过将实时泥浆测井数据与特征性钻屑和随钻测井(随钻测井)电缆数据整合起来而尽早发现这些衰落。由于结晶玄武岩骨架的高抗压强度,我们强调了玄武岩地层可能保持孔隙度和渗透率到比典型沉积物更大的深度。关键火山岩相的地下非均质分布通常包括硬,致密岩与软,弱火山岩的紧密混合和分层,这可能会促进埋藏压实过程中产生复杂的原地应力。发生这种情况时,井筒稳定性预测(如火山岩层的裂缝和井筒塌陷梯度)可能会与盆地等效沉积层序中的预期相差甚远。火山泥层膨胀,不稳定的火山碎屑序列和与侵入有关的壁架效应的例子被用来描述钻头和弦柱粘连的主要原因。如果要更好地进行钻前风险评估,成本预测,实时识别和缓解,则需要对包含火山层序的预期区域内遇到的钻探复杂性有更深入的了解。 (C)2016 Elsevier Ltd.保留所有权利。

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