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Response to “Reply to the comment on Zafar et al., 2025.”

14 min readJan 29, 2026

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1. Introduction

The reply by Zafar et al. (2026) to Bhat’s (2025) comment contains several assertions that warrant critical examination against contemporary research in Proto-Tethyan tectonics, back-arc basin evolution, slab dynamics, and S-type granite petrogenesis. This response presents evidence-based challenges to the authors’ interpretations, grounded in recent peer-reviewed literature (2022–2025).

2. The Sr Isotope Data Issue Requires Systematic Re-evaluation

2.1 Inadequate Data Quality Control

The authors’ dismissal of the 0.5678 initial ⁸⁷Sr/⁸⁶Sr value as merely from a “global comparison dataset” evades the fundamental issue: inclusion of geologically impossible data compromises the entire comparative framework. Wang et al. (2022) reported this value for sample 17GYB09 with a Rb/Sr ratio of 52, which the authors claim explains the anomaly. However, this explanation is scientifically problematic.

Contemporary evidence challenges this dismissal:

1. High Rb/Sr ratios alone cannot produce sub-mantle Sr isotope ratios.: Even extremely high Rb/Sr systems converge toward radiogenic (high ⁸⁷Sr/⁸⁶Sr) values over time, not depleted values below primordial mantle (Faure & Mensing, 2005; Dickin, 2018).

2. The value violates fundamental geochronological principles.: Shan et al. (2022)…

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A researcher studying isotope geochemistry. A gold medalist, DST-INSPIRE Fellow, and CSIR-NET qualified. Author, writer & an Instructor.