The Age and Exhumation Time of the Eastern Kamchatka Sedimentary Complexes Based on Apatite Track Dating

Pub Date : 2024-02-04 DOI:10.1134/s1819714023080122
N. V. Tsukanov, K. A. Dozorova
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Abstract

The paper presents and analyzes new and previously published data on track dating of detrital apatite grains isolated from different-age lithotectonic complexes of Eastern Kamchatka. The investigations were carried out in areas with different geodynamic settings: in Kronotsky Peninsula which is situated in the convergence zone of the Kamchatka margin with the relatively warm and light oceanic crust of the Pacific plate with the Obruchev Rise; in the Kamchatsky Peninsula situated in the collision zone of the Komandorsky block of the Aleutian volcanic arc and the Kamchatka continental margin; and the Kumroch Range, complexes of which belong to the Ozernoy–Valagin and Vetlovsky terranes. The analysis allowed us to distinguish several exhumation events: 29.9–34.9, 19.3–24.1, 10.2–15.4, 6.2–8.6, and 3.3–5.1 Ma. The highlighted age intervals correlate well with the main tectonic events and indicate that the accretionary and collisional processes in Eastern Kamchatka continued from the Oligocene to the Late Miocene–Pliocene.

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基于磷灰石轨道测定法的东堪察加沉积岩群的年龄和出露时间
本文介绍并分析了从堪察加半岛东部不同时代的岩构造复合体中分离出来的非晶质磷灰石颗粒的轨道测年新数据和以前发表的数据。调查是在具有不同地球动力学背景的地区进行的:克罗诺茨基半岛,位于堪察加半岛边缘与太平洋板块相对温暖、轻质的大洋地壳与奥布鲁切夫隆起的汇聚区;堪察加半岛,位于阿留申火山弧科曼多尔斯基地块与堪察加大陆边缘的碰撞区;以及库姆罗奇山脉,其中的复合体属于奥泽尔诺-瓦拉金和维特洛夫斯基地块。通过分析,我们可以区分出几个掘起事件:29.9-34.9、19.3-24.1、10.2-15.4、6.2-8.6 和 3.3-5.1 Ma。突出的年龄段与主要构造事件密切相关,表明东堪察加半岛的增生和碰撞过程从渐新世一直延续到晚中新世-更新世。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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