Magma processes and genesis of the Cretaceous Kawara granodiorite Ushikiri-yama body (Ushikiri-yama granodiorite), North Kyushu, SW Japan

Abstract

The Cretaceous Ushikiri-yama granodiorite is exposed in the northern part of Tagawa city (Fukuoka Prefecture, SW Japan) and is part of the North Kyushu batholith. Three types of dikes with varying compositions are associated with the Ushikiri-yama granodiorite: porphyritic fine-grained diorite (Pr Fine Di), porphyritic finegrained tonalite (Pr Fine To), and porphyritic fine-grained granite (Pr Fine Gr). The granodiorite intrudes the pre-Cretaceous basement rocks as an isolated stock, which can be divided into two bodies (North and South bodies), separated by a fine-grained granodiorite unit with a hypidiomorphic granular texture. The South body, which contains magmatic epidote, was intruded by the North body. Higher initial Sr isotope ratios of the South body, relative to the North body, indicate that sedimentary rocks were assimilated in the magma of the South body during its emplacement in the middle/upper crust. Geochemical data indicate that the Pr Fine To resulted from mixing of the magmas that produced the South body and the Pr Fine Di, with minor crustal contamination by host sedimentary rocks. Fractional crystallization of plagioclase, biotite, and hornblende in the South body resulted in the differentiation of the evolved Pr Fine Gr. In addition, Pr Fine Di has a sanukitic high-Mg andesite composition that is similar to Cretaceous high-Mg diorite bodies from the North Kyushu batholith. Overall, the results indicate that a variety of igneous processes including magma mixing, fractional crystallization, and assimilation with the host rocks, were responsible for the formation of the Ushikiri-yama granodiorite.

Petrogenesis of Josoji rhyolite and intrusive rocks of NE Shimane Peninsula, SW Japan: implication on Miocene volcanism related to back-arc rifting in San’in region

“…A relevant analogy can be drawn from the Cretaceous granitic intrusions, widely distributed across 200 x 200 km area on Kyushu Island in the southwestern Japan arc. Although almost all the granitic intrusions exhibit similar initial Sr and Nd isotopic compositions (e.g., Kagami, et al, 1992;Owada et al, 1999;Muraoka et al, 2020;Yuhara, et al, 2022), their origins are diverse from the mafic lower crust (e.g., Eshima et al, 2023) to the tonalitic middle crust (e.g., Kamei, 2002;Kamei et al, 2009). Hence, it is important to recognize that igneous rocks with similar initial Sr and Nd isotopic compositions do not necessarily share a common source material.…”

Anatomy of Shaku–dake high–Mg diorite, southwest Japan: Lithofacies variations and growth process of high–Mg diorite stock

“…The HBG is considered to be a member of the Kawaradake granodiorite, which is composed of several stocks (Fig. 1a; Murakami, 1985), and the intrusive ages are approximately 103 Ma based on the uraninite Th-U-Pb chemical and hornblende K-Ar ages (Yokoyama et al, 2016;Eshima et al, 2019). This age (103 Ma) overlaps with the magmatic period of the previously reported zircon U-Pb ages of the granitic rocks from the Cretaceous Northern Kyushu batholith (Adachi et al, 2012;Tiepolo et al, 2012;Miyazaki et al, 2017;Yuhara et al, 2019aYuhara et al, , 2019b.…”