Do Radioisotope Clocks Need Repair? Testing the Assumptions of Isochron Dating Using K-Ar, Rb-Sr, Sm-Nd, and Pb-Pb Isotopes

نویسنده

  • Steven A. Austin
چکیده

The assumptions of conventional whole-rock and mineral isochron radioisotope dating were tested using a suite of radioisotopes from two Precambrian rocks. Amphibolite from the Beartooth Mountains of Wyoming shows evidence of thorough metamorphism by isochemical processes from andesite by an early Precambrian magma-intrusion event. A diabase sill, exposed within the wall of Grand Canyon at Bass Rapids, formed by a rapid intrusion event. The event segregated minerals gravitationally, apparently starting from an isotopically homogeneous magma. Although K-Ar, Rb-Sr, Sm-Nd, and Pb-Pb methods ought to yield concordant isochron dates for each of these magmatic events, these four radioisotope pairs gave significantly discordant ages. Special allowance was made for larger-than-conventional uncertainties expressed as 2σ errors associated with the calculated “ages.” Within a single Beartooth amphibolite sample, three discordant mineral isochron “ages” range from 2515±110 Ma (Rb-Sr mineral isochron) to 2886±190 Ma (Sm-Nd mineral isochron). The diabase sill in Grand Canyon displays discordant isochron “ages” ranging from 841.5±164 Ma (K-Ar whole-rock isochron) to 1379±140 Ma (Sm-Nd mineral isochron). Although significant discordance exists between the K-Ar, Rb-Sr, Sm-Nd, and Pb-Pb radioisotope methods, each radioisotope pair appears to yield concordant “ages” internally between whole-rocks and minerals. Internal concordance is best illustrated from the Bass Rapids diabase sill by the tightly constrained Rb-Sr whole-rock and mineral * Chairman, Geology Department, Institute for Creation Research, Santee, California 326 Steven A. Austin isochron “ages” of 1055±46 Ma and 1060±24 Ma, respectively. The most problematic discordance is the Sm-Nd and Pb-Pb whole-rock and mineral isochron “ages” that significantly exceed the robust Rb-Sr whole-rock and mineral isochron “ages.” It could be argued that the robust Rb-Sr whole-rock and mineral isochron “ages” are in error, but an adequate explanation for the error has not been offered. The geological context of these Precambrian rocks places severe limitations on possible explanations for isochron discordance. Inheritance of minerals, slow cooling, and post-magmatic loss of daughter radioisotopes are not supported as processes causing isochron discordance in Beartooth amphibolite or Bass Rapids diabase. Recently, geochronologists researching the Great Dyke, a Precambrian layered mafic and ultramafic intrusion of Zimbabwe in southeast Africa, have documented a similar pattern of radioisotope discordance. Alpha-emitting radioisotopes (147Sm, 235U, and 238U) give older “ages” than β-emitting radioisotopes (87Rb and 40K) when applied to the same rocks. Therefore, it can be argued that a change in radioisotope decay rates in the past could account for these discordant isochron “ages” for the same geologic event. Conventional radioisotope clocks need repair.

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Uranium-lead Isotopic Systematics of the Martian Meteorite Zagami

Introduction: The crystallization age of Zagami has been well established by the Rb-Sr and Sm-Nd isochron techniques. Isotopic analysis on purified mineral fractions yield Rb-Sr ages of 178±3, 174±14, and 163±19 Ma [1-2], and a Sm-Nd age of 163±7 Ma [2]. Whole rock and leachate pairs have also been analyzed for U-Th-Pb isotopes and yield a Th-Pb age of 230±5 Ma and a U-Pb age of 229±8 Ma [3]. C...

متن کامل

The origin of geochemical diversity of lunar mantle sources inferred from the combined U–Pb, Rb–Sr, and Sm–Nd isotope systematics of mare basalt 10017

The results of our combined U–Pb, Rb–Sr, and Sm–Nd isotope study of mare basalt 10017 contribute to the understanding of the petrogenetic processes involved in the origin of geochemical diversity in lunar mare basalt sources, as well as the U–Pb isotope systematics of the Moon. The Rb–Sr, Sm–Nd, and U–Pb isotope systems yield concordant crystallization ages of 3.633 ± 0.057 Ga, 3.678 ± 0.069 Ga...

متن کامل

New Age Constraints on the Metamorphic Evolution of the High-Pressure/Low-Temperature Belt in the Western Tianshan Mountains, NW China

The western Tianshan high-pressure/low-temperature orogenic belt in NW China contains eclogite-facies metavolcanic rocks and omphacite-bearing blueschists. Previous Sm-Nd (omphacite, garnet, glaucophane, whole rock) and Ar/Ar (crossite) dating of eclogite-facies rocks has suggested an age of ca. 345 Ma as the best approximation for the timing of peak metamorphic conditions. The samples describe...

متن کامل

A combinedSm–Nd, Rb–Sr, and U–Pb isotopic study of Mg-suite norite 78238: Further evidence for early differentiation of the Moon

Lunar Mg-suite norite 78238 was dated using the Sm–Nd, Rb–Sr, and U–Pb isotopic systems in order to constrain the age of lunar magma ocean solidification and the beginning of Mg-suite magmatism, as well as to provide a direct comparison between the three isotopic systems. The Sm–Nd isotopic system yields a crystallization age for 78238 of 4334 ± 37 Ma and an initial e Nd value of 0.27 ± 0.74. T...

متن کامل

Constraints on the U-Pb isotopic systematics of Mars inferred from a combined U-Pb, Rb-Sr, and Sm-Nd isotopic study of the Martian meteorite Zagami

Uranium-lead, Rb-Sr, and Sm-Nd isotopic analyses have been performed on the same whole-rock, mineral, and leachate fractions of the basaltic martian meteorite Zagami to better constrain the U-Pb isotopic systematics of martian materials. Although the Rb-Sr and Sm-Nd systems define concordant crystallization ages of 166 6 Ma and 166 12 Ma, respectively, the U-Pb isotopic system is disturbed. Nev...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2005