|
miércoles, 16 de agosto de 2023
Updating our Google Account inactivity policy
lunes, 2 de mayo de 2022
Re: Your Outstanding Payment Notice
On Behalf of the Sub-Committee On Foreign Payment Reconciliation (SCFP), I write to inform you that your transaction has been investigated by us and the reason you have not received your long outstanding fund has been discovered.
Sequel to our investigation,it was discovered that the officials in charge of your payment are making this your transaction difficult for you with the aim of enriching themselves and the moment you became frustrated, they will now divert the fund into their personal pockets.
The officials do not have idea of what is currently going on between us because they will convince you more if they are allowed to be acquainted of this development. Once again, kindly desist communication with them instantly and Keep your transaction strictly confidential. Finally, Foreign Payment Reconciliation board have mandated this office to release your payment with immediate effect.
Sequel to the above, a payment instruction has been forwarded to our Accredited paying bank in China to enable them release the sum of one million five hundred thousand United States dollars (US1,500,000) in your favour from our reserved account with their bank as first installment and upon your confirmation of this first payment, your balance will be credited immediately.
For a satisfactory payment relief and acknowledgment, you are directed to forward your claim request and inquiries to the China Merchant Bank via this below operational Channel:
By reconfirming and forwarding to them your below information
(A) YOUR FULL NAME
(B) FULL ADDRESS
(C) YOUR DIRECT TELEPHONE LINE.
(D) COPY OF YOUR PASSPORT OR DRIVERS LICENSE (MEANS OF IDENTIFICATION)
THIS FIRST INSTALMENT: Five Hundred thousand United states dollars serve as a part-payment and also a test wire transfer into your bank account in other to avoid any foreign interference during the course of the transfer.
Thanks for your co-operation.
Scott Anthony
martes, 30 de noviembre de 2021
Learn more about our updated Terms of Service
|
miércoles, 16 de diciembre de 2020
Important policy changes for Google Account storage
|
martes, 25 de febrero de 2020
Learn more about our updated Terms of Service
|
lunes, 30 de enero de 2012
Changes to Google Privacy Policy and Terms of Service
Is this email not displaying properly? | ||||
Dear Google user, We're getting rid of over 60 different privacy policies across Google and replacing them with one that's a lot shorter and easier to read. Our new policy covers multiple products and features, reflecting our desire to create one beautifully simple and intuitive experience across Google. We believe this stuff matters, so please take a few minutes to read our updated Privacy Policy and Terms of Service at http://www.google.com/policies. These changes will take effect on March 1, 2012. | ||||
One policy, one Google experience | ||||
Easy to work across Google Our new policy reflects a single product experience that does what you need, when you want it to. Whether you're reading an email that reminds you to schedule a family get-together or finding a favorite video that you want to share, we want to ensure you can move across Gmail, Calendar, Search, YouTube, or whatever your life calls for with ease. | Tailored for you If you're signed into Google, we can do things like suggest search queries – or tailor your search results – based on the interests you've expressed in Google+, Gmail, and YouTube. We'll better understand which version of Pink or Jaguar you're searching for and get you those results faster. | Easy to share and collaborate When you post or create a document online, you often want others to see and contribute. By remembering the contact information of the people you want to share with, we make it easy for you to share in any Google product or service with minimal clicks and errors. | ||
| ||||
Protecting your privacy hasn't changed Our goal is to provide you with as much transparency and choice as possible, through products like Google Dashboard and Ads Preferences Manager, alongside other tools. Our privacy principles remain unchanged. And we'll never sell your personal information or share it without your permission (other than rare circumstances like valid legal requests). | Got questions? We've got answers. Visit our FAQ at http://www.google.com/policies/faq to read more about the changes. (We figured our users might have a question or twenty-two.) |
| ||
| ||||
Notice of Change March 1, 2012 is when the new Privacy Policy and Terms will come into effect. If you choose to keep using Google once the change occurs, you will be doing so under the new Privacy Policy and Terms of Service. Please do not reply to this email. Mail sent to this address cannot be answered. Also, never enter your Google Account password after following a link in an email or chat to an untrusted site. Instead, go directly to the site, such as mail.google.com or www.google.com/accounts. Google will never email you to ask for your password or other sensitive information. |
lunes, 3 de noviembre de 2008
a) El Magma (Introducción)
En el magma aparecen en suspensión diferentes tipos de cristales y fragmentos de rocas parcialmente fundidas, así como carbonatos, sulfuros y distintos componentes volátiles disueltos.
La interacción de las diversas condiciones físicas determina las características del magma, tanto en lo que se refiere a su composición química como a su viscosidad, resistencia, plasticidad y movimiento.
Tipos de magmas
Una primera clasificación de los distintos tipos de magmas hace referencia a su contenido en sílice. Los magmas con más de un 60% de anhídrido silícico son los llamados ácidos, mientras que los que poseen menos de dicha cantidad se denominan básicos.
Cuando el magma se proyecta al exterior por los puntos más débiles de la corteza terrestre, las masas de magma dan origen a los volcanes y forman, por enfriamiento, las rocas magmáticas, también llamadas ígneas o eruptivas, cuyo grado de cristalización es variable, y entre las que se encuentran el granito, el basalto o los pórfidos.
El ascenso de los magmas depende de sus condiciones físico-químicas (viscosidad, densidad, contenido en elementos volátiles, etc.), de las particularidades tectónicas de la región donde se encuentran y de las rocas que han de atravesar.
Los magmas ácidos son ligeros y viscosos, ascienden con facilidad y originan grandes depósitos.
Los magmas básicos, de mayor densidad, son menos viscosos y ascienden con mayor dificultad que los anteriores.
Densidad
Pequeñas diferencias composicionales pueden producir cambios de densidad sustanciales. Los fundidos basálticos, andesíticos y riolíticos en sus temperaturas de liquidus tienen densidades de 2.7,2.5 y 2.3 gm/cm3 , respectivamente. Los cambios de densidad asociados al enfriamiento son más pequeños que los cambios de densidad provocados por la diferenciación desde un líquido basáltico a uno riolítico.
La densidad de un fundido disminuye durante el enfriamiento, debido a la cristalización que separa del fundido los elementos más densos.los volátiles tienen un efecto importante sobre la densidad, por ejemplo el agua que llega a bajar la densidad del fluido.
Un fundido rico en sílice, como la riolita, está compuesto por cadenas largas, anillos y tetraedros de sílice. En consecuencia, los fundidos riolíticos tienen viscosidades muy altas, mientras que los basálticos tienen viscosidades mucho más bajas. La viscosidad también depende fuertemente de la temperatura.
El efecto de la presión es todavía desconocido, pero algunos datos experimentales indican un descenso de la viscosidad con el incremento de la presión.