新墨西哥州的氦气——地质分布、资源需求和勘探可能性

Q4 Earth and Planetary Sciences
R. Broadhead
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引用次数: 21

摘要

自1943年以来,新墨西哥州就开始生产氦气。位于新墨西哥州西北部Four Corners平台的8个油气田已经开始生产。在圣胡安县的Four Corners平台上,已经从Permian、pennsylvania、mickey和泥盆纪的储层中开采了近950 MMCF(百万立方英尺)的氦气。在新墨西哥州西北部,天然气中氦气含量的升高不仅发生在Four Corners平台的古生界储层中,也发生在Four Corners平台东部圣胡安盆地深层的古生界储层中。圣胡安盆地深部与前寒武纪基底相偏移的正交组高角度断裂是将氦从基底源输送到上覆古生代储层的运移通道。在二叠纪盆地的新墨西哥部分,大多数储层气体中的氦气浓度明显低于0.1%,因此尚未从产出气体中提取氦气。然而,在盆地西北侧的宾夕法尼亚和二叠纪储层中,氦含量在0.3 - 1.0%之间。氦来源于前寒武纪花岗岩中铀和钍的放射性衰变,并通过区域高角度走滑断层垂直运移到宾夕法尼亚和二叠系储层中。已知的富氦气体聚集在这些断层附近。下二叠世蒸发岩提供垂直断层封闭性。本区下、中古生界地层厚度仅几百英尺,导致前寒武纪烃源层与含氦储层之间的垂直运移距离较短。断裂走向确定了勘探走向。新墨西哥州的其他盆地和地区以富氦气体为特征,具有重要的勘探价值。这些地区包括该州中部索科罗东部的Chupadera Mesa地区和林肯县西部,该州中东部的Tucumcari盆地,以及该州中西部的Catron和Cibola县南部的广阔地区。在这些地区的宾夕法尼亚和二叠纪气体中发现了高水平的氦气。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Helium in New Mexico--geologic distribution, resource demand, and exploration possiblities
Helium gas has been produced in New Mexico since 1943. Production has been from eight oil and gas fields located on the Four Corners platform of northwestern New Mexico. Almost 950 MMCF (million cubic feet) helium has been produced from reservoirs of Permian, Pennsylvanian, Mississippian, and Devonian age on the Four Corners platform in San Juan County. In northwest New Mexico, elevated levels of helium in natural gases occur not only in Paleozoic reservoirs on the Four Corners platform but also in Paleozoic reservoirs in the deeper parts of the San Juan Basin located east of the Four Corners platform. The orthogonal sets of high-angle faults that offset Precambrian basement throughout the deeper parts of the San Juan Basin acted as migration pathways that transmitted helium from its basement source into overlying Paleozoic reservoirs. Helium has not been extracted from produced gases in the New Mexico part of the Permian Basin where the concentration of helium in most reservoir gases is significantly less than 0.1%. However, gases with helium contents ranging from 0.3 to almost 1.0% occur in Pennsylvanian and Permian reservoirs along the northwest flank of the basin. The helium appears to have originated by radiogenic decay of uranium and thorium in Precambrian granitic rocks and migrated vertically into Pennsylvanian and Permian reservoirs through regional, high-angle, strike-slip faults. Known accumulations of helium-rich gases are located near these faults. Lower Permian evaporites provide vertical fault seals. In this area, lower and middle Paleozoic strata are only a few hundred feet thick, resulting in short vertical migration distances between the Precambrian source and helium-bearing reservoirs. The fault trends define exploration fairways. Other basins and areas in New Mexico are characterized by helium-rich gases and are of significant exploratory interest. These areas include the Chupadera Mesa region of eastern Socorro and western Lincoln Counties in the central part of the state, the Tucumcari Basin in the east-central part of the state, and a wide region across Catron and southern Cibola Counties in the westcentral part of the state. Elevated levels of helium are found in Pennsylvanian and Permian gases in these areas.
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来源期刊
New Mexico Geology
New Mexico Geology Earth and Planetary Sciences-Geology
CiteScore
0.60
自引率
0.00%
发文量
0
期刊介绍: New Mexico Geology is a quarterly, peer-reviewed journal available by subscription. Articles of original research are generally less than 10,000 words in length and pertain to the geology of New Mexico and neighboring states, primarily for an audience of professional geologists or those with an interest in the geologic story behind the landscape. The journal also publishes abstracts from regional meetings, theses, and dissertations (NM schools), descriptions of new publications, book reviews, and upcoming meetings. Research papers, short articles, and abstracts from selected back issues of New Mexico Geology are now available as free downloads in PDF format. Back issues are also available in hard copy for a nominal fee.
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