没有证据表明Ojo Alamo砂岩与Nacimiento组之间存在整合接触

T. Williamson, S. Brusatte, D. Peppe, Ross Secord, A. Weil
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引用次数: 0

摘要

新墨西哥州西北部的圣胡安盆地是一个通过白垩纪-古近纪(K-Pg)边界沉积的Laramide盆地。然而,位于圣胡安盆地K-Pg边界附近的Ojo Alamo Ss的确切年龄仍然存在争议。确定其年龄对于了解该地区K-Pg边界附近的构造和生物历史至关重要。根据对Barrel Springs附近Bisti/De-na-zin Wash地区(BDNZ)这些地层的研究,先前的工作人员认为Ojo Alamo Ss的顶部和Nacimiento Fm的底部相互交错,因此是整合的。基于这种解释,大多数工人认为Ojo Alamo Ss(在这里被认为是在有限的意义上;BDNZ的Kimbeto段)为早古新世。Nacimiento Fm的基底与C29n相关,并产生了早古新世哺乳动物。这为底层的Ojo Alamo Ss提供了一个最低年龄。考虑到这个最低年龄限制,工人通常会在Ojo Alamo Ss的精确年龄中选择两种位置之一:(1)Ojo Alamo Ss跨越C29r的上部,或者(2)它仅限于C29n的下部。为了解决这个问题并确定Ojo Alamo s的更精确的年龄,我们研究了Ojo Alamo s与BDNZ上覆的Nacimiento Fm之间的地层关系。与以往的解释相反,我们发现这种地层接触不整合。相反,其他工作人员认为是“Ojo Alamo砂岩的上部”,它与Nacimiento Fm的基底部分相连,实际上是Nacimiento Fm透镜状河道砂岩的残余物。这一重新解释表明,在BDNZ地区,Nacimiento Fm和Ojo Alamo Ss之间的地层接触可能代表了Ojo Alamo Ss与Nacimiento Fm底部之间长达0.5 Ma的巨大间隙。今后的工作应侧重于更准确地确定Ojo Alamo - Nacimiento地层接触的年龄和间断时间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
No evidence for conformable contact between the Ojo Alamo Sandstone and the Nacimiento Formation
The San Juan Basin of northwestern New Mexico is a Laramide basin that accumulated sediments through the Cretaceous-Paleogene (K-Pg) boundary. However, the precise age of the Ojo Alamo Ss which lies near the K-Pg boundary in the San Juan Basin, remains controversial. Determining its age is crucial to understanding the tectonic and biotic history near the K-Pg boundary in this area. Based on study of these strata in the Bisti/De-na-zin Wash area (BDNZ) near Barrel Springs, previous workers have argued that the top of the Ojo Alamo Ss and the base of the Nacimiento Fm are interfingering and therefore are conformable. Based on this interpretation, most workers have regarded the Ojo Alamo Ss (here regarded in the restricted sense; = Kimbeto Member) in the BDNZ to be early Paleocene in age. The base of the Nacimiento Fm has been correlated to C29n and produces early Paleocene mammals. This provides a minimum age for the underlying Ojo Alamo Ss. Given this minimum age constraint workers have generally taken one of two positions for the precise age of the Ojo Alamo Ss: (1) the Ojo Alamo Ss. spans the upper part of C29r, or (2) it is restricted to only the lower part of C29n. To resolve this question and to determine a more precise age for the Ojo Alamo Ss, we examined the stratigraphic relationships between the Ojo Alamo Ss and the overlying Nacimiento Fm in the BDNZ. Contrary to previous interpretations, we find that this formational contact is not conformable. Rather, what other workers have assumed to be the “upper part of Ojo Alamo Sandstone” that interfingers with basal parts of the Nacimiento Fm is actually a remnant of a lenticular channel sandstone of the Nacimiento Fm. This reinterpretation suggests that the formational contact between the Nacimiento Fm and the Ojo Alamo Ss may represent a significant hiatus of up to ~ 0.5 Ma separating the Ojo Alamo Ss from the base of the Nacimiento Fm in the BDNZ area. Future work should focus on more accurately determining the age and refining the duration of the hiatus at the Ojo Alamo – Nacimiento formational contact.
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