In situ U-Th-Pb geochronology was born some two decades ago with the introduction and development of high-resolution secondary ion mass spectrometry (SIMS or SHRIMP [Sensitive High Mass Resolution Ion MicroProbe]; Compston et al. 1984, Williams 1998, Compston 1999, Davis et al.; this volume, Ireland and Williams, this volume). This technique clearly demonstrate
Modern geochronology has moved beyond the acquisition of dates: the goal is to understand the signif...
The rapid advances in in situ laser ablation (LA) inductively coupled plasma-mass spectrometry (ICP-...
The need in geology for in situ U-Pb age determinations of minerals is illustrated by two examples: ...
The chronologic record encoded in accessory minerals, based on the radioactive decay of U and Th, is...
This paper reports new developments in in situ U–Pb zircon geochronology using 266 and 213 nm laser ...
In-situ analysis of zircons The systematics of U and Pb in zircons serve as one of the most importan...
Zircon (ZrSiO4) is the most commonly used mineral in U-Pb geochronology. Although it has proven to b...
The in situ Pb geochronological capabilities of a laser ablation-inductively coupled plasma-mass spe...
Zircon and other U-Th-Pb-bearing minerals are now recognized as key geochemical and geochronological...
Understanding the mechanisms that govern the evolution of magmatic systems necessitates a firm grasp...
Zircon (ZrSiO4) is the most commonly used mineral in U–Pb geochronology. Although it has proven to b...
is s fr ctiv d zir epth cou rod ate lum zirc — d r ablation-multicollector-inductively coupled plasm...
In this study we used LA-ICP-MS (laser ablation-inductively coupled plasma-mass spectrometry) to de...
Until recently, in situ U-Pb zircon geochronology could be carried out only using ion microprobes, r...
During the past 10–15 years, analytical innovations in geochronology have greatly enhanced the appli...
Modern geochronology has moved beyond the acquisition of dates: the goal is to understand the signif...
The rapid advances in in situ laser ablation (LA) inductively coupled plasma-mass spectrometry (ICP-...
The need in geology for in situ U-Pb age determinations of minerals is illustrated by two examples: ...
The chronologic record encoded in accessory minerals, based on the radioactive decay of U and Th, is...
This paper reports new developments in in situ U–Pb zircon geochronology using 266 and 213 nm laser ...
In-situ analysis of zircons The systematics of U and Pb in zircons serve as one of the most importan...
Zircon (ZrSiO4) is the most commonly used mineral in U-Pb geochronology. Although it has proven to b...
The in situ Pb geochronological capabilities of a laser ablation-inductively coupled plasma-mass spe...
Zircon and other U-Th-Pb-bearing minerals are now recognized as key geochemical and geochronological...
Understanding the mechanisms that govern the evolution of magmatic systems necessitates a firm grasp...
Zircon (ZrSiO4) is the most commonly used mineral in U–Pb geochronology. Although it has proven to b...
is s fr ctiv d zir epth cou rod ate lum zirc — d r ablation-multicollector-inductively coupled plasm...
In this study we used LA-ICP-MS (laser ablation-inductively coupled plasma-mass spectrometry) to de...
Until recently, in situ U-Pb zircon geochronology could be carried out only using ion microprobes, r...
During the past 10–15 years, analytical innovations in geochronology have greatly enhanced the appli...
Modern geochronology has moved beyond the acquisition of dates: the goal is to understand the signif...
The rapid advances in in situ laser ablation (LA) inductively coupled plasma-mass spectrometry (ICP-...
The need in geology for in situ U-Pb age determinations of minerals is illustrated by two examples: ...