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편집 파일: 1609659856.M60603P18615.server.saraya-global.com,S=11868,W=12059:2,

Envelope-to: jaisone@saraya.com.my
Delivery-date: Sun, 03 Jan 2021 15:44:16 +0800
To: <jaisone@saraya.com.my>
Message-ID: <5593875538102255921746241041@u7308.ebusboosr.us>
Date: Sat, 2 Jan 2021 23:43:25 -0800
From: "Opinion Rewards" <OpinionRewards@ebusboosr.us>
Content-Language: en-us
MIME-Version: 1.0
Content-Transfer-Encoding: 8bit
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 Content analysis details:   (24.6 points, 5.0 required)
  pts rule name              description
 ---- ---------------------- --------------------------------------------------
  1.0 BAYES_999              BODY: Bayes spam probability is 99.9 to 100%
                             [score: 1.0000]
  5.0 BAYES_99               BODY: Bayes spam probability is 99 to 100%
                             [score: 1.0000]
  1.2 URIBL_ABUSE_SURBL      Contains an URL listed in the ABUSE SURBL
                             blocklist
                             [URIs: ebusboosr.us]
  2.7 RCVD_IN_PSBL           RBL: Received via a relay in PSBL
                             [50.2.214.18 listed in psbl.surriel.com]
  0.0 HTML_MESSAGE           BODY: HTML included in message
  0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or
                             identical to background
  0.9 RAZOR2_CHECK           Listed in Razor2 (http://razor.sf.net/)
  1.9 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
                             [cf: 100]
  4.5 URIBL_DBL_SPAM         Contains a spam URL listed in the Spamhaus DBL
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                             [URIs: ebusboosr.us]
  0.1 URIBL_SBL_A            Contains URL's A record listed in the Spamhaus SBL
                             blocklist
                             [URIs: www.ebusboosr.us]
  0.8 CPANEL_LOTS_OF_EMPTY_LINE RAW: Spam that has large block of
                             empty lines
  0.8 KAM_INFOUSMEBIZ        Prevalent use of
                             .info|.us|.me|.me.uk|.biz|xyz|id|rocks|life
                              domains in spam/malware
  1.5 SUBJ_ILLEGAL_CHARS     Subject: has too many raw illegal characters
  2.0 RDNS_NONE              Delivered to internal network by a host with no rDNS
  1.0 KAM_LAZY_DOMAIN_SECURITY Sending domain does not have any
                             anti-forgery methods
  0.0 SUBJECT_NEEDS_ENCODING Subject is encoded but does not specify
                             the encoding
  0.0 FSL_BULK_SIG           Bulk signature with no Unsubscribe
  1.1 NORDNS_LOW_CONTRAST    No rDNS + hidden text
X-Spam-Flag: YES
Subject:  ***SPAM***  Take a Survey – Get $1,500 for Groceries!

------=Part.886.5592.1609659805
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Content-Type: text/plain; charset="UTF-8"

Take a Survey – Get $1,500 for Groceries!

If you have problem with view image you can, browse me

http://www.ebusboosr.us/l/lt4B559RK4VG/217CQ624RH1041W103EX55381022Q839046674

http://www.ebusboosr.us/l/lc5R559BV4DW/217YC624WP1041L103RK55381022D839046674

des range has many active volcanoes distributed in four volcanic zones separated by areas of inactivity. The Andean volcanism is a result of subduction of the Nazca Plate and Antarctic Plate underneath the South American Plate. The belt is subdivided into four main volcanic zones that are separated from each other by volcanic gaps. The volcanoes of the belt are diverse in terms of activity style, products and morphology. While some differences can be explained by which volcanic zone a volcano belongs to, there are significant differences inside volcanic zones and even between neighbouring volcanoes. Despite being a type location for calc-alkalic and subduction volcanism, the Andean Volcanic Belt has a large range of volcano-tectonic settings, such as rift systems and extensional zones, transpressional faults, subduction of mid-ocean ridges and seamount chains apart from a large range of crustal thicknesses and magma ascent paths, and different amount of crustal assimilations. Ore deposits and evaporates The Andes Mountains host large ore and salt deposits and some of their eastern fold and thrust belt acts as traps for commercially exploitable amounts of hydrocarbons. In the forelands of the Atacama Desert some of the largest porphyry copper mineralizations occurs making Chile and Peru the first and second largest exporters of copper in the world. Porphyry copper in the western slopes of the Andes has been generated by hydrothermal fluids (mostly water) during the cooling of plutons or volcanic systems. The porphyry mineralization further benefited from the dry climate that let them largely out of the disturbing actions of meteoric water. The dry climate in the central western Andes has also led to the creation of extensive saltpeter deposits which were extensively mined until the invention of synthetic nitrates. Yet another result of the dry climate are the salars of Atacama and Uyuni, the first one being the largest source of lithium today and the second the world's largest reserve of the element. Early Mesozoic and Neogene plutonism in Bolivia's Cordillera Central crea

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