Interrelationships between the upper coal member of the Menefee Formation, the La Ventana Tongue, and the Lewis Shale in the southeastern San Juan Basin

E. C. Beaumont, Gretchen K. Hoffman
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引用次数: 7

Abstract

-The La Yentana Tongue of the Cliff House Sandstone has been the subject of several studies in the northwest and central San Juan Basin, in particular for oil and gas potential. The lack of drill-hole dala in the southeastern San Juan Basin had restricted detailed studies in this area to outcrops and a few oil and gas test logs. Logs from the New Mexico Bureau of Mines and Mineral Resources coal-quality drilling program ( 1985-1988), additional oil and gas drilling completed since the late 1970s, together with the older data provide sufficient subsurface data for detailed interpretations of stratigraphic relationships in the southeastern San Juan Basin. A 27-km cross section based on 24 geophysical logs was constructed north-northeastward from the outcrop area, 8 km east of Torreon Trading Post. The cross section transects the upper coal member of the Menefee, the La Ventana Tongue and the Lewis Shale. The maximum development of the La Ventana Tongue is clearly seen on the cross section, as is the relationship of the La Ventana to the coals within the upper coal member sequence. After a sudden landward shift of the shoreline that terminated the La Ventana buildup, a secondary stacking of barrier beach sandstones developed further inland. This unit is informally referred to in this report as the Chacra Mesa tongue. The intertonguing between the upper coal member of the Menefee and the La Ventana Tongue can be related to the principle of stratidynamics. This concept assumes continuing subsidence in a depositional environment and deals with transitional units. such as the upper coal member and the La Yentana, between the nonmarine and marine. The variables introduced are rate of subsidence and rate of shoreline shift. The La Ventana-upper coal member sequence developed during a time of minimal shoreline movement, with minor oscillations and variable sediment
圣胡安盆地东南部Menefee组上部煤系、La Ventana舌与Lewis页岩的相互关系
在圣胡安盆地西北部和中部,Cliff House砂岩的La Yentana舌头一直是几项研究的主题,特别是石油和天然气潜力。由于圣胡安盆地东南部缺乏钻孔数据,该地区的详细研究仅限于露头和少量油气测试测井。新墨西哥矿业和矿产资源局煤炭质量钻探项目(1985-1988)的日志,自20世纪70年代末以来完成的额外石油和天然气钻探,以及较旧的数据,为详细解释圣胡安盆地东南部的地层关系提供了足够的地下数据。在Torreon Trading Post以东8公里处,从露头区向东北偏北方向,根据24条地球物理测井曲线构建了一条27公里的剖面。该剖面横切了Menefee、La Ventana舌和Lewis页岩的上部煤段。在剖面上可以清楚地看到拉文塔纳舌的最大发育,以及拉文塔纳与上部煤段层序内煤的关系。在海岸线突然向陆地移动,终止了拉文塔纳的堆积之后,第二次堆积的屏障海滩砂岩进一步向内陆发展。这个单位在本报告中被非正式地称为查克拉梅萨语。Menefee上煤系与La Ventana舌间舌的形成与地层动力学原理有关。这一概念假定在沉积环境中持续沉降,并处理过渡单元。如上部煤系和拉延塔纳,介于非海相和海相之间。引入的变量是沉降速率和岸线移动速率。拉文塔纳—上煤系层序发育于最小岸线运动时期,振荡较小,沉积变化较大
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